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  • 1
    Keywords: Anden ; Argentinien ; Gondwanaland ; Palöozoikum ; Argentina ; Geology ; Geology, Stratigraphic ; Gondwana (Continent) ; Paleozoic
    Description / Table of Contents: R. J. Pankhurst and C. W. Rapela: The proto-Andean margin of Gondwana: an introduction / Geological Society, London, Special Publications, 142:1-9, doi:10.1144/GSL.SP.1998.142.01.01 --- Ricardo A. Astini: Stratigraphical evidence supporting the rifting, drifting and collision of the Laurentian Precordillera terrane of western Argentina / Geological Society, London, Special Publications, 142:11-33, doi:10.1144/GSL.SP.1998.142.01.02 --- Martin Keller, Werner Buggisch, and Oliver Lehnert: The stratigraphical record of the Argentine Precordillera and its plate-tectonic background / Geological Society, London, Special Publications, 142:35-56, doi:10.1144/GSL.SP.1998.142.01.03 --- Juan L. Benedetto: Early Palaeozoic brachiopods and associated shelly faunas from western Gondwana: their bearing on the geodynamic history of the pre-Andean margin / Geological Society, London, Special Publications, 142:57-83, doi:10.1144/GSL.SP.1998.142.01.04 --- Patricia wood Dickerson and Martin Keller: The Argentine Precordillera: its odyssey from the Laurentian Ouachita margin towards the Sierras Pampeanas of Gondwana / Geological Society, London, Special Publications, 142:85-105, doi:10.1144/GSL.SP.1998.142.01.05 --- Warren D. Huff, Stig M. Bergström, Dennis R. Kolata, Carlos A. Cingolani, and Ricardo A. Astini: Ordovician K-bentonites in the Argentine Precordillera: relations to Gondwana margin evolution / Geological Society, London, Special Publications, 142:107-126, doi:10.1144/GSL.SP.1998.142.01.06 --- Heinrich Bahlburg: The geochemistry and provenance of Ordovician turbidites in the Argentine Puna / Geological Society, London, Special Publications, 142:127-142, doi:10.1144/GSL.SP.1998.142.01.07 --- Victor A. Ramos, R. D. Dallmeyer, and Graciela Vujovich: Time constraints on the Early Palaeozoic docking of the Precordillera, central Argentina / Geological Society, London, Special Publications, 142:143-158, doi:10.1144/GSL.SP.1998.142.01.08 --- Graciela I. Vujovich and Suzanne Mahlburg Kay: A Laurentian? Grenville-age oceanic arc/back-arc terrane in the Sierra de Pie de Palo, Western Sierras Pampeanas, Argentina / Geological Society, London, Special Publications, 142:159-179, doi:10.1144/GSL.SP.1998.142.01.09 --- C. W. Rapela, R. J. Pankhurst, C. Casquet, E. Baldo, J. Saavedra, C. Galindo, and C. M. Fanning: The Pampean Orogeny of the southern proto-Andes: Cambrian continental collision in the Sierras de Córdoba / Geological Society, London, Special Publications, 142:181-217, doi:10.1144/GSL.SP.1998.142.01.10 --- Luis H. Dalla Salda, Mónica G. López de Luchi, Carlos A. Cingolani, and Ricardo Varela: Laurentia-Gondwana collision: the origin of the Famatinian-Appalachian Orogenic Belt (a review) / Geological Society, London, Special Publications, 142:219-234, doi:10.1144/GSL.SP.1998.142.01.11 --- W. Von Gosen and C. Prozzi: Structural evolution of the Sierra de San Luis (Eastern Sierras Pampeanas, Argentina): implications for the Proto-Andean Margin of Gondwana / Geological Society, London, Special Publications, 142:235-258, doi:10.1144/GSL.SP.1998.142.01.12 --- J. P. Sims, T. R. Ireland, A. Camacho, P. Lyons, P. E. Pieters, R. G. Skirrow, P. G. Stuart-Smith, and R. Miró: U-Pb, Th-Pb and Ar-Ar geochronology from the southern Sierras Pampeanas, Argentina: implications for the Palaeozoic tectonic evolution of the western Gondwana margin / Geological Society, London, Special Publications, 142:259-281, doi:10.1144/GSL.SP.1998.142.01.13 --- J. Saavedra, A. Toselli, J. Rossi, E. Pellitero, and F. Durand: The Early Palaeozoic magmatic record of the Famatina System: a review / Geological Society, London, Special Publications, 142:283-295, doi:10.1144/GSL.SP.1998.142.01.14 --- Grady C. Grissom, Susan M. Debari, and Lawrence W. Snee: Geology of the Sierra de Fiambalá, northwestern Argentina: implications for Early Palaeozoic Andean tectonics / Geological Society, London, Special Publications, 142:297-323, doi:10.1144/GSL.SP.1998.142.01.15 --- E. J. Llambías, A. M. Sato, A. Ortiz Suárez, and C. Prozzi: The granitoids of the Sierra de San Luis / Geological Society, London, Special Publications, 142:325-341, doi:10.1144/GSL.SP.1998.142.01.16 --- R. J. Pankhurst, C. W. Rapela, J. Saavedra, E. Baldo, J. Dahlquist, I. Pascua, and C. M. Fanning: The Famatinian magmatic arc in the central Sierras Pampeanas: an Early to Mid-Ordovician continental arc on the Gondwana margin / Geological Society, London, Special Publications, 142:343-367, doi:10.1144/GSL.SP.1998.142.01.17
    Pages: Online-Ressource (383 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1862390215
    Language: English
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  • 2
    Keywords: Mathematisches Modell ; Sedimentationsbecken ; Basins (Geology) ; Computer simulation ; Geologia econômica ; Geological modeling ; Geology ; Mathematical models ; Methodology ; Petroleum ; Petroleum - Geology ; Petróleo (modelos matemáticos) ; Prospecting ; Prospecção
    Description / Table of Contents: D. W. Waples: Basin modelling: how well have we done? / Geological Society, London, Special Publications, 141:1-14, doi:10.1144/GSL.SP.1998.141.01.01 --- M. R. Giles, S. L. Indrelid, and D. M. D. James: Compaction — the great unknown in basin modelling / Geological Society, London, Special Publications, 141:15-43, doi:10.1144/GSL.SP.1998.141.01.02 --- A. Okui, R. M. Siebert, and H. Matsubayashi: Simulation of oil expulsion by 1-D and 2-D basin modelling — saturation threshold and relative permeabilities of source rocks / Geological Society, London, Special Publications, 141:45-72, doi:10.1144/GSL.SP.1998.141.01.03 --- D. W. Waples and G. D. Couples: Some thoughts on porosity reduction — rock mechanics, overpressure and fluid flow / Geological Society, London, Special Publications, 141:73-81, doi:10.1144/GSL.SP.1998.141.01.04 --- T. Tokunaga, S. Hosoya, H. Tosaka, K. Kojima, and S. Hosoya: An estimation of the intrinsic permeability of argillaceous rocks and the effects on long-term fluid migration / Geological Society, London, Special Publications, 141:83-94, doi:10.1144/GSL.SP.1998.141.01.05 --- D. Darby, R. S. Haszeldine, and G. D. Couples: Central North Sea overpressures: insights into fluid flow from one- and two-dimensional basin modelling / Geological Society, London, Special Publications, 141:95-107, doi:10.1144/GSL.SP.1998.141.01.06 --- T. Throndsen and M. Wangen: A comparison between 1-D, 2-D and 3-D basin simulations of compaction, water flow and temperature evolution / Geological Society, London, Special Publications, 141:109-116, doi:10.1144/GSL.SP.1998.141.01.07 --- G. Archard, J. Stafford, K. Bardwell, M. Bagge, J. Stafford, and K. Bardwell: A review of techniques used to determine geological and thermal history in the Southern North Sea / Geological Society, London, Special Publications, 141:117-136, doi:10.1144/GSL.SP.1998.141.01.08 --- R. Schegg and W. Leu: Analysis of erosion events and palaeogeothermal gradients in the North Alpine Foreland Basin of Switzerland / Geological Society, London, Special Publications, 141:137-155, doi:10.1144/GSL.SP.1998.141.01.09 --- J. A. Hegre, J. L. Pittion, J. P. Herbin, and N. V. Lopatin: Geochemical modelling in an organic-rich source rock: the Bazhenov Formation / Geological Society, London, Special Publications, 141:157-167, doi:10.1144/GSL.SP.1998.141.01.10 --- W. A. Symington, K. E. Green, J. Huang, R. J. Pottorf, and L. L. Summa: A multidisciplinary approach to modelling secondary migration: a Central North Sea example / Geological Society, London, Special Publications, 141:169-185, doi:10.1144/GSL.SP.1998.141.01.11 --- T. T. Y. Ho, R. P. Jensen, S. K. Sahai, R. H. Leadholm, and O. Senneseth: Comparative studies of pre- and post-drilling modelled thermal conductivity and maturity data with post-drilling results: implications for basin modelling and hydrocarbon exploration / Geological Society, London, Special Publications, 141:187-208, doi:10.1144/GSL.SP.1998.141.01.12 --- R. O. Thomsen: Aspects of applied basin modelling: sensitivity analysis and scientific risk / Geological Society, London, Special Publications, 141:209-221, doi:10.1144/GSL.SP.1998.141.01.13 --- K. Gallagher and D. W. Morrow: A novel approach for constraining heat flow histories in sedimentary basins / Geological Society, London, Special Publications, 141:223-239, doi:10.1144/GSL.SP.1998.141.01.14
    Pages: Online-Ressource (VIII, 245 Seiten) , Diagramme, Karten
    ISBN: 1862390088
    Language: English
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  • 3
    Keywords: Lyell, Charles ; Rezeption ; Biography ; Geologie ; Geologists ; Geologists - Great Britain - Biography ; Geology ; Geology - History
    Description / Table of Contents: Derek J. Blundell and Andrew C. Scott: Introduction / Geological Society, London, Special Publications, 143:vii-viii, doi:10.1144/GSL.SP.1998.143.01.01 --- Part 1. The Life and Influence of Lyell --- M. J. S. Rudwick: Lyell and the Principles of Geology / Geological Society, London, Special Publications, 143:1-15, doi:10.1144/GSL.SP.1998.143.01.02 --- John C. Thackray: Charles Lyell and the Geological Society / Geological Society, London, Special Publications, 143:17-20, doi:10.1144/GSL.SP.1998.143.01.03 --- Leonard G. Wilson: Lyell: the man and his times / Geological Society, London, Special Publications, 143:21-37, doi:10.1144/GSL.SP.1998.143.01.04 --- Ezio Vaccari: Lyell’s reception on the continent of Europe: a contribution to an open historiographical problem / Geological Society, London, Special Publications, 143:39-52, doi:10.1144/GSL.SP.1998.143.01.05 --- Robert H. Dott, Jr: Charles Lyell’s debt to North America: his lectures and travels from 1841 to 1853 / Geological Society, London, Special Publications, 143:53-69, doi:10.1144/GSL.SP.1998.143.01.06 --- Gerald M. Friedman: Charles Lyell in New York State / Geological Society, London, Special Publications, 143:71-81, doi:10.1144/GSL.SP.1998.143.01.07 --- Claudine Cohen: Charles Lyell and the evidences of the antiquity of man / Geological Society, London, Special Publications, 143:83-93, doi:10.1144/GSL.SP.1998.143.01.08 --- Part 2. Lyell and the Development of Geological Science --- M. R. Leeder: Lyell’s Principles of Geology: foundations of sedimentology / Geological Society, London, Special Publications, 143:95-110, doi:10.1144/GSL.SP.1998.143.01.09 --- William A. Berggren: The Cenozoic Era: Lyellian (chrono)stratigraphy and nomenclatural reform at the millennium / Geological Society, London, Special Publications, 143:111-132, doi:10.1144/GSL.SP.1998.143.01.10 --- A. Hallam: Lyell’s views on organic progression, evolution and extinction / Geological Society, London, Special Publications, 143:133-136, doi:10.1144/GSL.SP.1998.143.01.11 --- Joe D. Burchfield: The age of the Earth and the invention of geological time / Geological Society, London, Special Publications, 143:137-143, doi:10.1144/GSL.SP.1998.143.01.12 --- Patrick J. Boylan: Lyell and the dilemma of Quaternary glaciation / Geological Society, London, Special Publications, 143:145-159, doi:10.1144/GSL.SP.1998.143.01.13 --- James Rodger Fleming: Charles Lyell and climatic change: speculation and certainty / Geological Society, London, Special Publications, 143:161-169, doi:10.1144/GSL.SP.1998.143.01.14 --- Victor R. Baker: Catastrophism and uniformitarianism: logical roots and current relevance in geology / Geological Society, London, Special Publications, 143:171-182, doi:10.1144/GSL.SP.1998.143.01.15 --- John Mather: From William Smith to William Whitaker: the development of British hydrogeology in the nineteenth century / Geological Society, London, Special Publications, 143:183-196, doi:10.1144/GSL.SP.1998.143.01.16 --- Part 3. The Legacy of Lyell --- C. R. Van Staal, J. F. Dewey, C. Mac Niocaill, and W. S. McKerrow: The Cambrian-Silurian tectonic evolution of the northern Appalachians and British Caledonides: history of a complex, west and southwest Pacific-type segment of Iapetus / Geological Society, London, Special Publications, 143:197-242, doi:10.1144/GSL.SP.1998.143.01.17 --- Andrew C. Scott: The legacy of Charles Lyell: advances in our knowledge of coal and coal-bearing strata / Geological Society, London, Special Publications, 143:243-260, doi:10.1144/GSL.SP.1998.143.01.18 --- J. H. Calder: The Carboniferous evolution of Nova Scotia / Geological Society, London, Special Publications, 143:261-302, doi:10.1144/GSL.SP.1998.143.01.19 --- R. C. L. Wilson: Sequence stratigraphy: a revolution without a cause? / Geological Society, London, Special Publications, 143:303-314, doi:10.1144/GSL.SP.1998.143.01.20 --- Christopher J. Talbot: Extrusions of Hormuz salt in Iran / Geological Society, London, Special Publications, 143:315-334, doi:10.1144/GSL.SP.1998.143.01.21 --- Hazel Rymer, Fabrizio Ferrucci, and Corinne A. Locke: Mount Etna: monitoring in the past, present and future / Geological Society, London, Special Publications, 143:335-347, doi:10.1144/GSL.SP.1998.143.01.22 --- Bruce A. Bolt: Earthquakes and Earth structure: a perspective since Hutton and Lyell / Geological Society, London, Special Publications, 143:349-361, doi:10.1144/GSL.SP.1998.143.01.23 --- John Knill: Humanity and the modern environment / Geological Society, London, Special Publications, 143:363-368, doi:10.1144/GSL.SP.1998.143.01.24
    Pages: Online-Ressource (VIII, 376 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1862390185
    Language: English
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  • 4
    Keywords: Wessex ; England ; Großbritannien ; Becken (Geologie) ; Entstehung ; Entwicklung ; Erdölgeologie ; Erdöllagerstätte ; Erdgaslagerstätte ; Geologie ; Tektonik ; Petroleum ; Geology ; England ; Wessex Basin ; fossile Brennstoffe
    Description / Table of Contents: John R. Underhill and Robert Stoneley: Introduction to the development, evolution and petroleum geology of the Wessex Basin / Geological Society, London, Special Publications, 133:1-18, doi:10.1144/GSL.SP.1998.133.01.01 --- Hydrocarbon Habitat --- James G. Buchanan: The exploration history and controls on hydrocarbon prospectivity in the Wessex basins, southern England, UK / Geological Society, London, Special Publications, 133:19-37, doi:10.1144/GSL.SP.1998.133.01.02 --- P. W. Hawkes, A. J. Fraser, and C. C. G. Einchcomb: The tectono-stratigraphic development and exploration history of the Weald and Wessex basins, Southern England, UK / Geological Society, London, Special Publications, 133:39-65, doi:10.1144/GSL.SP.1998.133.01.03 --- Malcolm Butler: The geological history of the southern Wessex Basin — a review of new information from oil exploration / Geological Society, London, Special Publications, 133:67-86, doi:10.1144/GSL.SP.1998.133.01.04 --- Stratigraphic Syntheses --- Nigel R. Ainsworth, William Braham, F. John Gregory, Ben Johnson, and Christopher King: A proposed latest Triassic to earliest Cretaceous microfossil biozonation for the English Channel and its adjacent areas / Geological Society, London, Special Publications, 133:87-102, doi:10.1144/GSL.SP.1998.133.01.05 --- Nigel R. Ainsworth, William Braham, F. John Gregory, Ben Johnson, and Christopher King: The lithostratigraphy of the latest Triassic to earliest Cretaceous of the English Channel and its adjacent areas / Geological Society, London, Special Publications, 133:103-164, doi:10.1144/GSL.SP.1998.133.01.06 --- David C. Cole and Ian C. Harding: Use of palynofacies analysis to define Lower Jurassic (Sinemurian to Pliensbachian) genetic stratigraphic sequences in the Wessex Basin, England / Geological Society, London, Special Publications, 133:165-185, doi:10.1144/GSL.SP.1998.133.01.07 --- Regional Studies --- Adam Law: Regional uplift in the English Channel: quantification using sonic velocity / Geological Society, London, Special Publications, 133:187-197, doi:10.1144/GSL.SP.1998.133.01.08 --- Richard J. Bray, Ian R. Duddy, and Paul F. Green: Multiple heating episodes in the Wessex Basin: implications for geological evolution and hydrocarbon generation / Geological Society, London, Special Publications, 133:199-213, doi:10.1144/GSL.SP.1998.133.01.09 --- Neil A. McMahon and Jonathan Turner: The documentation of a latest Jurassic-earliest Cretaceous uplift throughout southern England and adjacent offshore areas / Geological Society, London, Special Publications, 133:215-240, doi:10.1144/GSL.SP.1998.133.01.10 --- Structural Studies --- Michael J. Harvey and Simon A. Stewart: Influence of salt on the structural evolution of the Channel Basin / Geological Society, London, Special Publications, 133:241-266, doi:10.1144/GSL.SP.1998.133.01.11 --- C. Smith and I. R. Hatton: Inversion tectonics in the Lyme Bay-West Dorset area of the Wessex Basin, UK / Geological Society, London, Special Publications, 133:267-281, doi:10.1144/GSL.SP.1998.133.01.12 --- H. S. Beeley and M. G. Norton: The structural development of the Central English Channel High — constraints from section restoration / Geological Society, London, Special Publications, 133:283-298, doi:10.1144/GSL.SP.1998.133.01.13 --- R. Hunsdale, D. J. Sanderson, and R. Hunsdale: Fault size distribution analysis — an example from Kimmeridge Bay, Dorset, UK / Geological Society, London, Special Publications, 133:299-310, doi:10.1144/GSL.SP.1998.133.01.14 --- M. Miliorizos and A. Ruffell: Kinematics of the Watchet-Cothelstone-Hatch Fault System: implications for the fault history of the Wessex Basin and adjacent areas / Geological Society, London, Special Publications, 133:311-330, doi:10.1144/GSL.SP.1998.133.01.15 --- Sedimentological Advances --- A. Ruffell: Tectonic accentuation of sequence boundaries: evidence from the Lower Cretaceous of southern England / Geological Society, London, Special Publications, 133:331-348, doi:10.1144/GSL.SP.1998.133.01.16 --- Stephen P. Hesselbo: Basal Wealden of Mupe Bay: a new model / Geological Society, London, Special Publications, 133:349-353, doi:10.1144/GSL.SP.1998.133.01.17 --- R. Goldring, T. R. Astin, J. E. A. Marshall, S. Gabbott, and C. D. Jenkins: Towards an integrated study of the depositional environment of the Bencliff Grit (Upper Jurassic) of Dorset / Geological Society, London, Special Publications, 133:355-372, doi:10.1144/GSL.SP.1998.133.01.18 --- Petroleum Geochemistry --- M. Ashley Bigge and Paul Farrimond: Biodegradation of seep oils in the Wessex Basin — a complication for correlation / Geological Society, London, Special Publications, 133:373-386, doi:10.1144/GSL.SP.1998.133.01.19 --- M. A. Parfitt and P. Farrimond: The Mupe Bay oil seep: a detailed organic geochemical study of a controversial outcrop / Geological Society, London, Special Publications, 133:387-397, doi:10.1144/GSL.SP.1998.133.01.20 --- Oil Field Case Histories --- T. McKie, J. Aggett, and A. J. C. Hogg: Reservoir architecture of the upper Sherwood Sandstone, Wytch Farm field, southern England / Geological Society, London, Special Publications, 133:399-406, doi:10.1144/GSL.SP.1998.133.01.21 --- Jonathan Evans, David Jenkins, and Jon Gluyas: The Kimmeridge Bay oilfield: an enigma demystified / Geological Society, London, Special Publications, 133:407-413, doi:10.1144/GSL.SP.1998.133.01.22
    Pages: Online-Ressource (VI, 420 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799993
    Language: English
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  • 5
    Keywords: Nordafrika ; Erdölgeologie ; Lagerstätte ; Erdgas ; Erdöl ; Erdöllagerstätte ; Erdgaslagerstätte ; Geologie ; Tektonik ; Atlas (Gebirge) ; Kohlenwasserstoffe ; Petroleum ; Geology ; Africa, North ; fossile Brennstoffe ; Exploration und Prospektion von Bodenschätzen
    Description / Table of Contents: Duncan S. Macgregor: Introduction / Geological Society, London, Special Publications, 132:1-6, doi:10.1144/GSL.SP.1998.132.01.01 --- Palaeozoic and Sub-Salt Regional Papers --- David R. D. Boote, Daniel D. Clark-Lowes, and Marc W. Traut: Palaeozoic petroleum systems of North Africa / Geological Society, London, Special Publications, 132:7-68, doi:10.1144/GSL.SP.1998.132.01.02 --- Marc W. Traut, David R. D. Boote, and Daniel D. Clark-Lowes: Exploration history of the Palaeozoic petroleum systems of North Africa / Geological Society, London, Special Publications, 132:69-78, doi:10.1144/GSL.SP.1998.132.01.03 --- Duncan S. Macgregor: Giant fields, petroleum systems and exploration maturity of Algeria / Geological Society, London, Special Publications, 132:79-96, doi:10.1144/GSL.SP.1998.132.01.04 --- B. Fekirine and H. Abdallah: Palaeozoic lithofacies correlatives and sequence stratigraphy of the Saharan Platform, Algeria / Geological Society, London, Special Publications, 132:97-108, doi:10.1144/GSL.SP.1998.132.01.05 --- K. Echikh: Geology and hydrocarbon occurrences in the Ghadames Basin, Algeria, Tunisia, Libya / Geological Society, London, Special Publications, 132:109-129, doi:10.1144/GSL.SP.1998.132.01.06 --- Paul Logan and Ian Duddy: An investigation of the thermal history of the Ahnet and Reggane Basins, Central Algeria, and the consequences for hydrocarbon generation and accumulation / Geological Society, London, Special Publications, 132:131-155, doi:10.1144/GSL.SP.1998.132.01.07 --- Palaeozoic Reservoirs and Fields --- Rob Crossley and Neil McDougall: Lower Palaeozoic reservoirs of North Africa / Geological Society, London, Special Publications, 132:157-166, doi:10.1144/GSL.SP.1998.132.01.08 --- Mohamed Robert Djarnia and Berrached Fekirine: Sedimentological and diagenetic controls on Cambro-Ordovician reservoir quality in the southern Hassi Messaoud area (Saharan Platform, Algeria) / Geological Society, London, Special Publications, 132:167-174, doi:10.1144/GSL.SP.1998.132.01.09 --- N. Alem, S. Assassi, S. Benhebouche, and B. Kadi: Controls on hydrocarbon occurrence and productivity in the F6 reservoir, Tin Fouyé-Tabankort area, NW Illizi Basin / Geological Society, London, Special Publications, 132:175-186, doi:10.1144/GSL.SP.1998.132.01.10 --- Rabah Chaouchi, M. S. Malla, and F. Kechou: Sedimentological evolution of the Givetian-Eifelian (F3) sand bar of the West Alrar field, Illizi Basin, Algeria / Geological Society, London, Special Publications, 132:187-200, doi:10.1144/GSL.SP.1998.132.01.11 --- Mesozoic-Cenozoic Regional Papers --- Duncan S. Macgregor and Richard T. J. Moody: Mesozoic and Cenozoic petroleum systems of North Africa / Geological Society, London, Special Publications, 132:201-216, doi:10.1144/GSL.SP.1998.132.01.12 --- R. Guiraud: Mesozoic rifting and basin inversion along the northern African Tethyan margin: an overview / Geological Society, London, Special Publications, 132:217-229, doi:10.1144/GSL.SP.1998.132.01.13 --- M. Wilson, R. Guiraud, C. Moreau, and Y. J.-C. Bellion: Late Permian to Recent magmatic activity on the African-Arabian margin of Tethys / Geological Society, London, Special Publications, 132:231-263, doi:10.1144/GSL.SP.1998.132.01.14 --- M. L. Keeley and M. S. Massoud: Tectonic controls on the petroleum geology of NE Africa / Geological Society, London, Special Publications, 132:265-281, doi:10.1144/GSL.SP.1998.132.01.15 --- Al Moundir Morabet, Rabah Bouchta, and Haddou Jabour: An overview of the petroleum systems of Morocco / Geological Society, London, Special Publications, 132:283-296, doi:10.1144/GSL.SP.1998.132.01.16 --- Moesozoic Reservoirs and Fields --- S. M. Richardson, N. Vivian, R. J. Cook, M. Wilkes, and H. Hussein: Application of fault seal analysis techniques in the Western Desert, Egypt / Geological Society, London, Special Publications, 132:297-315, doi:10.1144/GSL.SP.1998.132.01.17 --- Rutger Gras and Bindra Thusu: Trap architecture of the Early Cretaceous Sarir Sandstone in the eastern Sirt Basin, Libya / Geological Society, London, Special Publications, 132:317-334, doi:10.1144/GSL.SP.1998.132.01.18 --- D. Spring and O. P. Hansen: The influence of platform morphology and sea level on the development of a carbonate sequence: the Harash Formation, Eastern Sirt Basin, Libya / Geological Society, London, Special Publications, 132:335-353, doi:10.1144/GSL.SP.1998.132.01.19 --- R. G. Loucks, R. T. J. Moody, J. K. Bellis, and A. A. Brown: Regional depositional setting and pore network systems of the El Garia Formation (Metlaoui Group, Lower Eocene), offshore Tunisia / Geological Society, London, Special Publications, 132:355-374, doi:10.1144/GSL.SP.1998.132.01.20 --- A. Zaïer, A. Beji-Sassi, S. Sassi, and R. T. J. Moody: Basin evolution and deposition during the Early Paleogene in Tunisia / Geological Society, London, Special Publications, 132:375-393, doi:10.1144/GSL.SP.1998.132.01.21 --- The Atlas Fold Belt --- R. Bracène, A. Bellahcène, D. Bekkouche, E. Mercier, and D. Frizon de Lamotte: The thin-skinned style of the South Atlas Front in Central Algeria / Geological Society, London, Special Publications, 132:395-404, doi:10.1144/GSL.SP.1998.132.01.22 --- Mark A. Morgan, John Grocott, and Richard T. J. Moody: The structural evolution of the Zaghouan-Ressas Structural Belt, northern Tunisia / Geological Society, London, Special Publications, 132:405-422, doi:10.1144/GSL.SP.1998.132.01.23 --- Karim Mekireche, Nordine Sabaou, and Reda-Samy Zazoun: Critical factors in the exploration of an Atlas intramontane basin; the Western Hodna Basin of northern Algeria / Geological Society, London, Special Publications, 132:423-432, doi:10.1144/GSL.SP.1998.132.01.24
    Pages: Online-Ressource (442 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1862390045
    Language: English
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  • 6
    Keywords: Südostasien ; Erdölgeologie ; Erdöl ; fossile Brennstoffe ; Geologie ; Kohlenwasserstofflagerstätte ; Geology ; Petroleum ; Southeast Asia
    Description / Table of Contents: A. J. Fraser and S. J. Matthews: Petroleum geology of SE Asia: an introduction / Geological Society, London, Special Publications, 126:1-2, doi:10.1144/GSL.SP.1997.126.01.01 --- Chris Sladen: Energy trends in SE Asia / Geological Society, London, Special Publications, 126:3-10, doi:10.1144/GSL.SP.1997.126.01.02 --- Robert Hall: Cenozoic plate tectonic reconstructions of SE Asia / Geological Society, London, Special Publications, 126:11-23, doi:10.1144/GSL.SP.1997.126.01.03 --- S. P. Todd, M. E. Dunn, and A. J. G. Barwise: Characterizing petroleum charge systems in the tertiary of SE Asia / Geological Society, London, Special Publications, 126:25-47, doi:10.1144/GSL.SP.1997.126.01.04 --- Chris Sladen: Exploring the lake basins of east and southeast Asia / Geological Society, London, Special Publications, 126:49-76, doi:10.1144/GSL.SP.1997.126.01.05 --- Coen T. A. M. Leo: Exploration in the Gulf of Thailand in deltaic reservoirs, related to the Bongkot Field / Geological Society, London, Special Publications, 126:77-87, doi:10.1144/GSL.SP.1997.126.01.06 --- S. J. Matthews, A. J. Fraser, S. Lowe, S. P. Todd, and F. J. Peel: Structure, stratigraphy and petroleum geology of the SE Nam Con Son Basin, offshore Vietnam / Geological Society, London, Special Publications, 126:89-106, doi:10.1144/GSL.SP.1997.126.01.07 --- R. H. Worden, M. J. Mayall, and I. J. Evans: Predicting reservoir quality during exploration: lithic grains, porosity and permeability in Tertiary clastic rocks of the South China Sea basin / Geological Society, London, Special Publications, 126:107-115, doi:10.1144/GSL.SP.1997.126.01.08 --- M. J. Mayall, A. Bent, and D. M. Roberts: Miocene carbonate buildups offshore Socialist Republic of Vietnam / Geological Society, London, Special Publications, 126:117-120, doi:10.1144/GSL.SP.1997.126.01.09 --- A. Wight, H. Friestad, I. Anderson, P. Wicaksono, and C. H. Reminton: Exploration history of the offshore Southeast Sumatra PSC, Java Sea, Indonesia / Geological Society, London, Special Publications, 126:121-142, doi:10.1144/GSL.SP.1997.126.01.10 --- Craig Schiefelbein and Nick Cameron: Sumatra/Java oil families / Geological Society, London, Special Publications, 126:143-146, doi:10.1144/GSL.SP.1997.126.01.11 --- J. M. Cole and S. Crittenden: Early Tertiary basin formation and the development of Lacustrine and quasi-lacustrine/marine source rocks on the Sunda Shelf of SE Asia / Geological Society, London, Special Publications, 126:147-183, doi:10.1144/GSL.SP.1997.126.01.12 --- Alastair Beach, J. Lawson Brown, Paul J. Brockbank, Steven D. Knott, Jean E. McCallum, and Alastair I. Welbon: Fault seal analysis of SE Asian basins with examples from West Java / Geological Society, London, Special Publications, 126:185-194, doi:10.1144/GSL.SP.1997.126.01.13 --- D. J. Prosser and R. R. Carter: Permeability heterogeneity within the Jerudong Formation: an outcrop analogue for subsurface Miocene reservoirs in Brunei / Geological Society, London, Special Publications, 126:195-235, doi:10.1144/GSL.SP.1997.126.01.14 --- I. C. Mat-Zin and R. E. Swarbrick: The tectonic evolution and associated sedimentation history of Sarawak Basin, eastern Malaysia: a guide for future hydrocarbon exploration / Geological Society, London, Special Publications, 126:237-245, doi:10.1144/GSL.SP.1997.126.01.15 --- M. E. J. Wilson and D. W. J. Bosence: Platform-top and ramp deposits of the Tonasa Carbonate Platform, Sulawesi, Indonesia / Geological Society, London, Special Publications, 126:247-279, doi:10.1144/GSL.SP.1997.126.01.16 --- P. J. Boult: A review of the petroleum potential of Papua New Guinea with a focus on the eastern Papuan Basin and the Pale Sandstone as a potential reservoir fairway / Geological Society, London, Special Publications, 126:281-291, doi:10.1144/GSL.SP.1997.126.01.17 --- J. B. Blanche and J. D. Blanche: An overview of the hydrocarbon potential of the Spratly Islands archipelago and its implications for regional development / Geological Society, London, Special Publications, 126:293-310, doi:10.1144/GSL.SP.1997.126.01.18 --- Ian M. Longley: The tectonostratigraphic evolution of SE Asia / Geological Society, London, Special Publications, 126:311-339, doi:10.1144/GSL.SP.1997.126.01.19 --- D. Roques, S. J. Matthews, and C. Rangin: Constraints on strike-slip motion from seismic and gravity data along the Vietnam margin offshore Da Nang: implications for hydrocarbon prospectivity and opening of the East Vietnam Sea / Geological Society, London, Special Publications, 126:341-353, doi:10.1144/GSL.SP.1997.126.01.20 --- A. J. McCarthy and C. F. Elders: Cenozoic deformation in Sumatra: oblique subduction and the development of the Sumatran Fault System / Geological Society, London, Special Publications, 126:355-363, doi:10.1144/GSL.SP.1997.126.01.21 --- Chris Howells: Tertiary response to oblique subduction and indentation in Sumatra, Indonesia: new ideas for hydrocarbon exploration / Geological Society, London, Special Publications, 126:365-374, doi:10.1144/GSL.SP.1997.126.01.22 --- John L. C. Chambers and Timothy E. Daley: A tectonic model for the onshore Kutai Basin, East Kalimantan / Geological Society, London, Special Publications, 126:375-393, doi:10.1144/GSL.SP.1997.126.01.23 --- Steve J. Moss, John Chambers, Ian Cloke, Dharma Satria, Jason R. Ali, Simon Baker, John Milsom, and Andy Carter: New observations on the sedimentary and tectonic evolution of the Tertiary Kutai Basin, East Kalimantan / Geological Society, London, Special Publications, 126:395-416, doi:10.1144/GSL.SP.1997.126.01.24 --- John Milsom, Robert Holt, Dzazali Bin Ayub, and Ross Smail: Gravity anomalies and deep structural controls at the Sabah-Palawan margin, South China Sea / Geological Society, London, Special Publications, 126:417-427, doi:10.1144/GSL.SP.1997.126.01.25
    Pages: Online-Ressource (VI, 436 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799918
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  • 7
    Keywords: Känozoikum ; Vortiefe ; Westeuropa ; Basins (Geology) ; Europe, Western ; Cenozoic ; Europe ; Geology ; Geology, Stratigraphic
    Description / Table of Contents: B. Durand: Foreword / Geological Society, London, Special Publications, 134:vii-viii, doi:10.1144/GSL.SP.1998.134.01.01 --- Alain Mascle and Cai Puigdefàbregas: Tectonics and sedimentation in foreland basins: results from the Integrated Basin Studies project / Geological Society, London, Special Publications, 134:1-28, doi:10.1144/GSL.SP.1998.134.01.02 --- Guadalquivir and Ebro Foreland Basins (Spain) --- M. Fernàndez, X. Berástegui, C. Puig, D. García-Castellanos, M. J. Jurado, M. Torné, and C. Banks: Geophysical and geological constraints on the evolution of the Guadalquivir foreland basin, Spain / Geological Society, London, Special Publications, 134:29-48, doi:10.1144/GSL.SP.1998.134.01.03 --- X. Berástegui, C.J. Banks, C. Puig, C. Taberner, D. Waltham, and M. Fernàndez: Lateral diapiric emplacement of Triassic evaporites at the southern margin of the Guadalquivir Basin, Spain / Geological Society, London, Special Publications, 134:49-68, doi:10.1144/GSL.SP.1998.134.01.04 --- Edward A. Williams, Mary Ford, Jaume Vergés, and Andrea Artoni: Alluvial gravel sedimentation in a contractional growth fold setting, Sant Llorenç de Morunys, southeastern Pyrenees / Geological Society, London, Special Publications, 134:69-106, doi:10.1144/GSL.SP.1998.134.01.05 --- J. Vergés, M. Marzo, T. Santaeulària, J. Serra-Kiel, D. W. Burbank, J. A. Muñoz, and J. Giménez-Montsant: Quantified vertical motions and tectonic evolution of the SE Pyrenean foreland basin / Geological Society, London, Special Publications, 134:107-134, doi:10.1144/GSL.SP.1998.134.01.06 --- Wouter Nijman: Cyclicity and basin axis shift in a piggyback basin: towards modelling of the Eocene Tremp-Ager Basin, South Pyrenees, Spain / Geological Society, London, Special Publications, 134:135-162, doi:10.1144/GSL.SP.1998.134.01.07 --- Anna Travé, Pierre Labaume, Francesc Calvet, Albert Soler, Jordi Tritlla, Martine Buatier, Jean-Luc Potdevin, Michel Séguret, Suzanne Raynaud, and Louis Briqueu: Fluid migration during Eocene thrust emplacement in the south Pyrenean foreland basin (Spain): an integrated structural, mineralogical and geochemical approach / Geological Society, London, Special Publications, 134:163-188, doi:10.1144/GSL.SP.1998.134.01.08 --- French Western Alps --- W. Henry Lickorish and Mary Ford: Sequential restoration of the external Alpine Digne thrust system, SE France, constrained by kinematic data and synorogenic sediments / Geological Society, London, Special Publications, 134:189-211, doi:10.1144/GSL.SP.1998.134.01.09 --- Andrea Artoni and Lawrence D. Meckel III: History and deformation rates of a thrust sheet top basin: the Barrême basin, western Alps, SE France / Geological Society, London, Special Publications, 134:213-237, doi:10.1144/GSL.SP.1998.134.01.10 --- Yann Philippe, Eric Deville, and Alain Mascle: Thin-skinned inversion tectonics at oblique basin margins: example of the western Vercors and Chartreuse Subalpine massifs (SE France) / Geological Society, London, Special Publications, 134:239-262, doi:10.1144/GSL.SP.1998.134.01.11 --- Christian Beck, Eric Deville, Eric Blanc, Yann Philippe, and Marc Tardy: Horizontal shortening control of Middle Miocene marine siliciclastic accumulation (Upper Marine Molasse) in the southern termination of the Savoy Molasse Basin (northwestern Alps/southern Jura) / Geological Society, London, Special Publications, 134:263-278, doi:10.1144/GSL.SP.1998.134.01.12 --- Swiss, German and Austrian Molasse Basin --- Martin Burkhard and Anna Sommaruga: Evolution of the western Swiss Molasse basin: structural relations with the Alps and the Jura belt / Geological Society, London, Special Publications, 134:279-298, doi:10.1144/GSL.SP.1998.134.01.13 --- J. Zweigel, T. Aigner, and H. Luterbacher: Eustatic versus tectonic controls on Alpine foreland basin fill: sequence stratigraphy and subsidence analysis in the SE German Molasse / Geological Society, London, Special Publications, 134:299-323, doi:10.1144/GSL.SP.1998.134.01.14 --- J. Zweigel: Reservoir analogue modelling of sandy tidal sediments, Upper Marine Molasse, SW Germany, Alpine foreland basin / Geological Society, London, Special Publications, 134:325-337, doi:10.1144/GSL.SP.1998.134.01.15 --- Ludwig R. Wagner: Tectono-stratigraphy and hydrocarbons in the Molasse Foredeep of Salzburg, Upper and Lower Austria / Geological Society, London, Special Publications, 134:339-369, doi:10.1144/GSL.SP.1998.134.01.16 --- Numerical Modelling --- Stefan Bornholdt and Hildegard Westphal: Automation of stratigraphic simulations: quasi-backward modelling using genetic algorithms / Geological Society, London, Special Publications, 134:371-379, doi:10.1144/GSL.SP.1998.134.01.17 --- Taco den Bezemer, Henk Kooi, Yuri Podladchikov, and Sierd Cloetingh: Numerical modelling of growth strata and grain-size distributions associated with fault-bend folding / Geological Society, London, Special Publications, 134:381-401, doi:10.1144/GSL.SP.1998.134.01.18 --- B. Andeweg and S. Cloetingh: Flexure and ‘unflexure’ of the North Alpine German-Austrian Molasse Basin: constraints from forward tectonic modelling / Geological Society, London, Special Publications, 134:403-422, doi:10.1144/GSL.SP.1998.134.01.19
    Pages: Online-Ressource (VIII, 427 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1862390150
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  • 8
    Keywords: Erdgasgeologie ; Erdölgeologie ; Nordsee, Süd ; Geology ; North Sea ; Petroleum ; Petroleum in submerged lands
    Description / Table of Contents: Karen Ziegler, Peter Turner, and Stephen Daines: Introduction / Geological Society, London, Special Publications, 123:1-3, doi:10.1144/GSL.SP.1997.123.01.01 --- K. W. Glennie: History of exploration in the southern North Sea / Geological Society, London, Special Publications, 123:5-16, doi:10.1144/GSL.SP.1997.123.01.02 --- K. W. Glennie: Recent advances in understanding the southern North Sea Basin: a summary / Geological Society, London, Special Publications, 123:17-29, doi:10.1144/GSL.SP.1997.123.01.03 --- Gareth T. George and Jeremy K. Berry: Permian (Upper Rotliegend) synsedimentary tectonics, basin development and palaeogeography of the southern North Sea / Geological Society, London, Special Publications, 123:31-61, doi:10.1144/GSL.SP.1997.123.01.04 --- John Howell and Nigel Mountney: Climatic cyclicity and accommodation space in arid to semi-arid depositional systems: an example from the Rotliegend Group of the UK southern North Sea / Geological Society, London, Special Publications, 123:63-86, doi:10.1144/GSL.SP.1997.123.01.05 --- Gregory P. Leveille, Rob Knipe, Colin More, Dave Ellis, Graham Dudley, Greg Jones, Quentin J. Fisher, and Gareth Allinson: Compartmentalization of Rotliegendes gas reservoirs by sealing faults, Jupiter Fields area, southern North Sea / Geological Society, London, Special Publications, 123:87-104, doi:10.1144/GSL.SP.1997.123.01.06 --- Gregory P. Leveille, Tim J. Primmer, Graham Dudley, David Ellis, and Gareth J. Allinson: Diagenetic controls on reservoir quality in Permian Rotliegendes sandstones, Jupiter Fields area, southern North Sea / Geological Society, London, Special Publications, 123:105-122, doi:10.1144/GSL.SP.1997.123.01.07 --- Nick Cameron and Tom Ziegler: Probing the lower limits of a fairway: further pre-Permian potential in the southern North Sea / Geological Society, London, Special Publications, 123:123-141, doi:10.1144/GSL.SP.1997.123.01.08 --- David G. Quirk and John F. Aitken: The structure of the Westphalian in the northern part of the southern North Sea / Geological Society, London, Special Publications, 123:143-152, doi:10.1144/GSL.SP.1997.123.01.09 --- D. G. Quirk: Sequence stratigraphy of the Westphalian in the northern part of the Southern North Sea / Geological Society, London, Special Publications, 123:153-168, doi:10.1144/GSL.SP.1997.123.01.10 --- F. C. J. Mijnssen: Modelling of sandbody connectivity in the Schooner Field / Geological Society, London, Special Publications, 123:169-180, doi:10.1144/GSL.SP.1997.123.01.11 --- C. S. Yang and Y. A. Baumfalk: Application of high-frequency cycle analysis in high-resolution sequence stratigraphy / Geological Society, London, Special Publications, 123:181-203, doi:10.1144/GSL.SP.1997.123.01.12
    Pages: Online-Ressource (209 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799829
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  • 9
    Unknown
    London : The Geological Society
    Keywords: Europa ; Kohle ; Kohlengeologie ; Technologie ; Coal ; Coal mines and mining ; Coal trade ; Europe ; Geology
    Description / Table of Contents: Dr Rod Gayer and Professor Jiri Pesek: Preface / Geological Society, London, Special Publications, 125:vii-viii, doi:10.1144/GSL.SP.1997.125.01.01 --- Regional Coal Reserves, Coal Basin Tectonics and Stratigraphy --- Josef Doruška: The Czech Republic energy policy: conception and implementation in a market economy / Geological Society, London, Special Publications, 125:1-2, doi:10.1144/GSL.SP.1997.125.01.02 --- J. Pešek and M. Dopita: Coal production and usage in the Czech Republic / Geological Society, London, Special Publications, 125:3-12, doi:10.1144/GSL.SP.1997.125.01.03 --- O. Kumpera: Controls on the evolution of the Namurian paralic basin, Bohemian Massif, Czech Republic / Geological Society, London, Special Publications, 125:13-27, doi:10.1144/GSL.SP.1997.125.01.04 --- Miroslav Krs, Jiří Pešek, Petr Pruner, Vladimír Skoček, and Jana Slepičková: The origin of magnetic remanence components of Westphalian C to Stephanian C sediments, West Bohemia: a record of waning Variscan tectonism / Geological Society, London, Special Publications, 125:29-47, doi:10.1144/GSL.SP.1997.125.01.05 --- Roland Dreesen, Dominique Bossiroy, Rudy Swennen, Jacques Thorez, Aurelio Fadda, Luciano Ottelli, and Eddy Keppens: A depositional and diagenetic model for the Eocene Sulcis coal basin of SW Sardinia / Geological Society, London, Special Publications, 125:49-75, doi:10.1144/GSL.SP.1997.125.01.06 --- H. İnaner and E. Nakoman: Turkish lignite deposits / Geological Society, London, Special Publications, 125:77-99, doi:10.1144/GSL.SP.1997.125.01.07 --- A. I. Karayigit and M. K. G. Whateley: The origin and properties of a coal seam associated with continental thin micritic limestones, Selimoglu-Divrigi, Turkey / Geological Society, London, Special Publications, 125:101-114, doi:10.1144/GSL.SP.1997.125.01.08 --- A. I. Karayigit and M. K. G. Whateley: Chemical characteristics, mineralogical composition and rank of high sulphur coking coals of Middle Miocene age in the Gökler coal field, Gediz, Turkey / Geological Society, London, Special Publications, 125:115-130, doi:10.1144/GSL.SP.1997.125.01.09 --- Nicolae Ţicleanu and Dorina Diaconiţǎ: The main coal facies and lithotypes of the Pliocene coal basin, Oltenia, Romania / Geological Society, London, Special Publications, 125:131-139, doi:10.1144/GSL.SP.1997.125.01.10 --- George D. Šiškov: Bulgarian low rank coals: geology and petrology / Geological Society, London, Special Publications, 125:141-148, doi:10.1144/GSL.SP.1997.125.01.11 --- I. E. Stukalova: Coal petrology and facies associations of the South Yakutian Coal Basin, Siberia / Geological Society, London, Special Publications, 125:149-160, doi:10.1144/GSL.SP.1997.125.01.12 --- Coal Petrology and Palaeontology --- Rod Gayer, Richard Fowler, and Gareth Davies: Coal rank variations with depth related to major thrust detachments in the South Wales coalfield: implications for fluid flow and mineralization / Geological Society, London, Special Publications, 125:161-178, doi:10.1144/GSL.SP.1997.125.01.13 --- J. Dvořák, J. Honěk, J. Pešek, and P. Valterová: Deep borehole evidence for a southward extension of the Early Namurian deposits near Němčičky, S. Moravia, Czech Republic: implication for rapid coalification / Geological Society, London, Special Publications, 125:179-193, doi:10.1144/GSL.SP.1997.125.01.14 --- Irena Kostova, Kalinka Markova, and Krasimir Kuntchev: Mössbauer spectroscopic investigation of low rank coal lithotypes / Geological Society, London, Special Publications, 125:195-199, doi:10.1144/GSL.SP.1997.125.01.15 --- P. I. Premović, R. S. Nikolić, and M. P. Premović: Comparison of solid state 13C NMR of algal coals/anthracite and charcoal-like fusinites: further evidence for graphitic domains / Geological Society, London, Special Publications, 125:201-205, doi:10.1144/GSL.SP.1997.125.01.16 --- Ivana Sýkorová, Jaroslav Černý, Helena Pavlíková, and Zuzana Weishauptová: Composition and properties of North Bohemian coals / Geological Society, London, Special Publications, 125:207-217, doi:10.1144/GSL.SP.1997.125.01.17 --- Maya Stefanova and Caroline Magnier: Aliphatic biological markers in Miocene Maritza-Iztok lignite, Bulgaria / Geological Society, London, Special Publications, 125:219-228, doi:10.1144/GSL.SP.1997.125.01.18 --- Svetilana Syabryaj: Floristic characters of the upper coal-bearing formation in the Transcarpathians / Geological Society, London, Special Publications, 125:229-236, doi:10.1144/GSL.SP.1997.125.01.19 --- Mineral Matter in Coal and the Environment --- S. R. H. Baqri: The distribution of sulphur in the Palaeocene coals of the Sindh Province of Pakistan / Geological Society, London, Special Publications, 125:237-243, doi:10.1144/GSL.SP.1997.125.01.20 --- Paul F. Cavender and D. Alan Spears: Sulphur distribution in a multi-bed seam / Geological Society, London, Special Publications, 125:245-260, doi:10.1144/GSL.SP.1997.125.01.21 --- Vladimír Bouška, Jiří Pešek, and Karel Žák: Values of δ34S in iron disulphides of the North Bohemian Lignite Basin, Czech Republic / Geological Society, London, Special Publications, 125:261-267, doi:10.1144/GSL.SP.1997.125.01.22 --- G. Jankes, O. Cvetković, and T. Glumičić: Determination of different forms of sulphur in Yugoslav soft brown coals / Geological Society, London, Special Publications, 125:269-272, doi:10.1144/GSL.SP.1997.125.01.23 --- P. I. Premović, N. D. Nikolić, M. S. Pavlović, LJ. S. Jovanović, and M. P. Premović: Origin of vanadium in coals: parts of the Western Kentucky (USA) No. 9 coal rich in vanadium / Geological Society, London, Special Publications, 125:273-286, doi:10.1144/GSL.SP.1997.125.01.24 --- D. A. Spears: Environmental impact of minerals in UK coals / Geological Society, London, Special Publications, 125:287-295, doi:10.1144/GSL.SP.1997.125.01.25 --- Mining Geophysics --- Vít Gregor and Antonín Těžký: A well logging method for the determination of the sulphur content of coal seams by means of deep gammaspectrometry / Geological Society, London, Special Publications, 125:297-307, doi:10.1144/GSL.SP.1997.125.01.26 --- Karel Mach: A logging correlation scheme for the Main coal seam of the North Bohemian brown coal basin, and the implications for the palaeogeographical development of the basin / Geological Society, London, Special Publications, 125:309-320, doi:10.1144/GSL.SP.1997.125.01.27 --- Karel Holub: Seismic monitoring for rockburst prevention in the Ostrava-Karviná Coalfield, Czech Republic / Geological Society, London, Special Publications, 125:321-328, doi:10.1144/GSL.SP.1997.125.01.28 --- Zdeněk Kaláb: An analysis of mining induced seismicity and its relationship to fault zones / Geological Society, London, Special Publications, 125:329-335, doi:10.1144/GSL.SP.1997.125.01.29 --- Stanislav Opluštil, Jiří Pešek, and Jiří Skopec: Comparison of structures derived from mine workings and those interpreted in seismic profiles: an example from the Kačice deposit, Kladno Mine, Bohemia / Geological Society, London, Special Publications, 125:337-347, doi:10.1144/GSL.SP.1997.125.01.30 --- Coal Technology and Coalbed Methane --- J. Barraza, M. Cloke, and A. Belghazi: Improvements in direct coal liquefaction using beneficiated coal fractions / Geological Society, London, Special Publications, 125:349-356, doi:10.1144/GSL.SP.1997.125.01.31 --- B. R. Aleksić, M. D. Ercegovac, O. G. Cvetković, B. Ž. Marković, T. L. Glumičić, B. D. Aleksić, and D. K. Vitorvić: Conversion of low rank coal into liquid fuels by direct hydrogenation / Geological Society, London, Special Publications, 125:357-363, doi:10.1144/GSL.SP.1997.125.01.32 --- R. Asmatulu, N. Acarkan, G. Onal, and M. S. Celik: Desulphurization of low-rank coals by low-temperature carbonization / Geological Society, London, Special Publications, 125:365-369, doi:10.1144/GSL.SP.1997.125.01.33 --- Michael K. G. Whateley, Zafer Gencer, and Ertem Tuncali: Amelioration of high organic sulphur coal for combustion in domestic stoves / Geological Society, London, Special Publications, 125:371-377, doi:10.1144/GSL.SP.1997.125.01.34 --- M. Stanojević, G. Jankes, M. Kuburović, M. Stanojević, and P. Blagojević: The use of pulverized lignite/natural gas mixed fuels in the high-temperature process of a cement rotary kiln / Geological Society, London, Special Publications, 125:379-383, doi:10.1144/GSL.SP.1997.125.01.35 --- Douchko Douchanov and Venecia Minkova: The possibility of underground gasification of Bulgarian Dobrudja’s coal / Geological Society, London, Special Publications, 125:385-390, doi:10.1144/GSL.SP.1997.125.01.36 --- E. L. Boardman and J. H. Rippon: Coalbed methane migration in and around fault zones / Geological Society, London, Special Publications, 125:391-408, doi:10.1144/GSL.SP.1997.125.01.37 --- V. Holub, M. Eliáš, P. Hrazdíra, and J. Franců: Geological research into gas sorbed in the coal seams of the Carboniferous in the Mšeno-Roudnice Basin, Czech Republic / Geological Society, London, Special Publications, 125:409-423, doi:10.1144/GSL.SP.1997.125.01.38 --- Ireneusz Grzybek, Lidia Gawlik, Wojciech Suwała, and Ryszard Kuzak: Method for estimating methane emissions from Polish coal mining / Geological Society, London, Special Publications, 125:425-434, doi:10.1144/GSL.SP.1997.125.01.39 --- G. Takla and Z. Vavrušák: Methane emission and its utilization from Ostrava-Karviná Collieries in the Upper Silesian coal basin, Czech Republic / Geological Society, London, Special Publications, 125:435-440, doi:10.1144/GSL.SP.1997.125.01.40
    Pages: Online-Ressource (VIII, 448 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799861
    Language: English
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  • 10
    Keywords: Speichergestein ; Strukturgeologie ; Failles (géologie) ; Faults (Geology) ; Geology ; Petroleum ; Pièges structuraux (Géologie pétrolière) ; Pétrole - Géologie ; Roches réservoirs (géologie pétrolière) ; Structural traps (Petroleum geology) ; Tectonique
    Description / Table of Contents: J. W. Cosgrove: The role of structural geology in reservoir characterization / Geological Society, London, Special Publications, 127:1-13, doi:10.1144/GSL.SP.1998.127.01.01 --- John Archer: Reservoir characterization and modelling: a framework for field development / Geological Society, London, Special Publications, 127:15-18, doi:10.1144/GSL.SP.1998.127.01.02 --- B. Freeman, G. Yielding, D. T. Needham, and M. E. Badley: Fault seal prediction: the gouge ratio method / Geological Society, London, Special Publications, 127:19-25, doi:10.1144/GSL.SP.1998.127.01.03 --- B. R. Crawford: Experimental fault sealing: shear band permeability dependency on cataclastic fault gouge characteristics / Geological Society, London, Special Publications, 127:27-47, doi:10.1144/GSL.SP.1998.127.01.04 --- Roy H. Gabrielsen, Randi-Kristin Aarland, and Einar Alsaker: Identification and spatial distribution of fractures in porous, siliciclastic sediments / Geological Society, London, Special Publications, 127:49-64, doi:10.1144/GSL.SP.1998.127.01.05 --- T. Manzocchi, P. S. Ringrose, and J. R. Underhill: Flow through fault systems in high-porosity sandstones / Geological Society, London, Special Publications, 127:65-82, doi:10.1144/GSL.SP.1998.127.01.06 --- Richard G. Gibson: Physical character and fluid-flow properties of sandstone-derived fault zones / Geological Society, London, Special Publications, 127:83-97, doi:10.1144/GSL.SP.1998.127.01.07 --- J. J. Walsh, J. Watterson, A. Heath, P. A. Gillespie, and C. Childs: Assessment of the effects of sub-seismic faults on bulk permeabilities of reservoir sequences / Geological Society, London, Special Publications, 127:99-114, doi:10.1144/GSL.SP.1998.127.01.08 --- Roderick J. Owen, Xiang-Yang Li, Colin D. Macbeth, and David C. Booth: Reservoir characterization: how can anisotropy help? / Geological Society, London, Special Publications, 127:115-119, doi:10.1144/GSL.SP.1998.127.01.09 --- L. Foley, T. S. Daltaban, and J. T. Wang: Numerical simulation of fluid flow in complex faulted regions / Geological Society, London, Special Publications, 127:121-132, doi:10.1144/GSL.SP.1998.127.01.10 --- S. A. Stewart and R. Podolski: Curvature analysis of gridded geological surfaces / Geological Society, London, Special Publications, 127:133-147, doi:10.1144/GSL.SP.1998.127.01.11 --- Gary D. Couples, Helen Lewis, and P. W. Geoff Tanner: Strain partitioning during flexural-slip folding / Geological Society, London, Special Publications, 127:149-165, doi:10.1144/GSL.SP.1998.127.01.12 --- Amgad I. Younes, Terry Engelder, and William Bosworth: Fracture distribution in faulted basement blocks: Gulf of Suez, Egypt / Geological Society, London, Special Publications, 127:167-190, doi:10.1144/GSL.SP.1998.127.01.13 --- Lidia Lonergan, Joe Cartwright, Rod Laver, and Joe Staffurth: Polygonal faulting in the Tertiary of the central North Sea: implications for reservoir geology / Geological Society, London, Special Publications, 127:191-207, doi:10.1144/GSL.SP.1998.127.01.14 --- R. K. Aarland and J. Skjerven: Fault and fracture characteristics of a major fault zone in the northern North Sea: analysis of 3D seismic and oriented cores in the Brage Field (Block 31/4) / Geological Society, London, Special Publications, 127:209-229, doi:10.1144/GSL.SP.1998.127.01.15 --- Haakon Fossen and Jonny Hesthammer: Structural geology of the Gullfaks Field, northern North Sea / Geological Society, London, Special Publications, 127:231-261, doi:10.1144/GSL.SP.1998.127.01.16
    Pages: Online-Ressource (VIII, 266 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799942
    Language: English
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  • 11
    facet.materialart.
    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-22
    Description: Im nördlichen Bereich der Provinz Kantabrien (Nordspanien) wurden Sedimente der "Mittelkreide" (Oberalb und Cenoman) unter stratigraphischen, faziellen und sedimentologi sehen Gesichtspunkten bearbeitet. Strukturell gehört die Region zum Nordkantabrischen Becken (NCB), dessen Einsenkung mit tektonischen Bewegungen im mittleren Valangin beginnt. Das NCB ist eines der zahlreichen Sedimentbecken, die sich infolge des mesozoischen Riftings und Spreadings in der Biscaya auf dem iberischen Nordschelf bilden. Strukturgeologisch zeigt das NCB eine E/W-Ausrichtung zwischen zwei Hochgebieten im S und N (Cabuemiga-Rücken und Liencres-Hoch), die als "Santillana-Achse" bezeichnet wird. Im W grenzt das NCB an das Paläozoikum des Asturischen Massivs. Östlich Santander wird es strukturell und faziell durch die N/S-streichende Rio-Miera-Flexur vom hochsubs identen Basko-Kantabrischen Becken abgetrennt. Die Sedimentation im NCB wird stark von tektonischen Ereignissen im sich bildenden Biscaya-Ozeans beeinflußt, durch welche die Strukturierung der Schichtenfolge in sedimentäre Megasequenzen erfolgt. Im Alb und Cenoman können folgende Megasequenz-Grenzen erkannt werden, durch welche die Megasequenzen des Alb und Cenoman definiert werden: • Santander-Tectoevent (Cenoman/Turon-Grenzbereich) • Vraconian Tectoevent (hohes Oberalb) • "Mittelalb-Ereignis" ("break-up unconformity", [?hohes] Unteralb). Das Mittelalb-Ereignis fuhrt im Arbeitsgebiet zum Zerbrechen der faziell wenig differenzierten Urgon-Karbonatplattformen des Clansay (Oberapt/Unteralb) in ostvergente Kippschollen. In den entstehenden N/S-orientierten Halbgräben werden im Mittelaib fluvio-deltaische Klastika abgelagert, während auf den Hochschollen eine Verkarstung erfolgt. Im tiefen Oberalb initiiert ein transgressiver Puls die weit verbreitete Ablagerung mariner Sedimente im NCB. Dieses transgressive Ereignis ist in ganz Iberien nachzuweisen. Im Laufe des Oberalb kommt es zu einem Onlap mariner Sedimente auch auf den ehemals emergenten Hochschollen und zu einem Ausgleich des durch das Mittelalb-Ereignis erzeugten Paläoreliefs. Durch weit verbreitete Emersion des NCB's infolge tektonischer Bewegungen im oberen Oberalb (Vraconian Tectoevent) wird die sedimentäre Megasequenz des Alb beendet. Die sedimentäre Megasequenz des Cenoman beginnt im Alb/Cenoman-Grenzbereich mit der Progradation deltaischer Klastika. Die im NCB der Santillana-Achse folgend von W nach E kanalisiert werden. Dieses "Santillana-Delta" mündet im Bereich Galizano/Langre östlich Santander in das Basko-Kantabrische Becken und verzahnt sich dort mit den Prodelta-Sedimenten des Valmaseda-Deltas ("Schwarzer Flysch" der Bilbao-Region). Die differentielle Subsidenz im NCB in Folge des Vraconian Tectoevents wird von den Delta-Sedimenten ausgeglichen. Im tiefen Untercenoman (untere Mantelliceras mantelli-Zone) gestaltet eine bedeutende transgressive Faziesentwicklung das gesamte NCB in einen vollmarinen, karbonatisch dominierten Ablagerungsraum um. Dieser transgressive Puls dürfte mit der "Untercenoman-Transgression" sensu lato korrelieren. Im Cenoman können folgende Ammoniten-Biozonen erkannt werden: • Obercenoman: Eucalycoceras pentagonum-Zone, und Metoicoceras geslinianum-Zone [pars] • Mittel cenoman: [Cunningtoniceras inerme-Zone], Acanthoceras rhotomagense-Zone und A. jukesbrownei-Zone • Untercenoman: Mantelliceras mantelli-Zone und M. dixoni-Zone. Das höchste Obercenoman (oberer Teil der geslinianum-Zone und die Neocardioceras juddii-Zone) fehlt im NCB. In der oberen mantelli-Zonc des NCB etabliert sich in weiten Bereichen die flachmarine Karbonat-Fazies der Altamira-Plattform, die sich östlich der Rio-Miera-Flexur mit mächtigen Beckensedimenten (Mergel, Knollenkalke, Kalk/Mergel-Rhythmite) verzahnt. Im Mittel- bis unteren Obercenoman wird die Altamira-Plattform in drei Schritten von E nach W "ertränkt". Die prominenten Drowning-Unconformities (mineralisierte Hartgründe mit Ammoniten) werden dabei stufenweise nach W jünger. Im Obercenoman (pentagonum-Zono) ist die gesamte Altamira-Plattform ertränkt und weite Teile des NCB werden in die Beckensedimentation einbezogen. Die Ablagerungsgeschichte des Cenoman wird durch das Santander-Tectoevent in der oberen geslinianum-Zonc beendet, infolgedessen weite Teile des NCB trockenfallen. Selbst in hochsubsidenten Beckenprofilen ist der Cenoman/Turon-Grenzbereich durch eine Schicht lücke gekennzeichnet. Die fazielle Entwicklung der cenomanen Megasequenz ist durch die schubweise voranschreitende ("pulsierende") Cenoman-Transgression geprägt. Insgesamt können im Cenoman sechs Sequenzgrenzen (SB's) erkannt werden, durch die die Ablagerungssequenzen DS Ce I bis VI definiert werden. Ihre stratigraphischen Positionen sind: • SB Ce VI = obere geslinianum-Zonc • SB Ce V = Wende Mittel/Obercenoman • SB Ce IV = basale jukesbrownei-Zone • SB Ce III = hohe dixoni-Zone • SB Ce II = obere mantelli-Zone • SB Ce I = untere mantelli-Zone. Im regionalen Vergleich zeigt sich für das Cenoman eine gute Übereinstimmung mit sequentiellen Gliederungen aus dem Basko-Kantabrischen Raum. Überregionale Vergleiche dokumentieren, daß viele der Meeresspiegel-Bewegungen im Cenoman (z.B. SB Ce III, mfz in der rhotomagense-Zone, SB Ce IV, HST in der pentagonum-Zone) über weite Entfernungen korreliert werden können und wahrscheinlich eustatische Signale darstellen. Die Korrelation mit der "globalen Meeresspiegel-Kurve" (Exxon Chart) ist schlecht. Betrachtet man die im Cenoman im NCB abgelagerten Sedimente als "2nd-order cycle", so zeigt sich ein übergeordneter transgressiver Trend mit einem maximalen Onlap im Obercenoman innerhalb der mfz von DS Ce VI (pentagonum-Zone). Das NCB zeigt im Oberalb und Cenoman im biogeographischen Vergleich starke tethyale Einflüsse. Das Turrilites scheuchzerianus/Neohibolites ultimus-Evert. im tiefen Mittelcenoman des NCB korreliert in bio-, sequenz- und Isotopen-stratigraphischer Hinsicht mit dem Actinocamax primus-Event NW-Europas, womit eine eventstratigraphische Anbindung an das "temperierte" Cenoman erreicht werden kann.
    Description: Mid-Cretaceous (Upper Albian and Cenomanian) sediments in the northern part of the province of Cantabria (northern Spain) were investigated with the emphasis on stratigraphical and sedimentological aspects. Structurally, the area belongs to the North Cantabrian Basin (NCB), the depositional history of which started with distensional tectonic movements in the Mid-Valanginian. The NCB is one of the numerous sedimentary basins which developed on the north Iberian continental margin in consequence of the rifting and spreading in the Bay of Biscay during Mesozoic times. It is a gulf-like basin with an E/W-elongation ("Santillana axis"). In the south and in the north the NCB is bordered by the Cabuemiga Ridge and the Liencres High, respectively. To the west, the NCB is bordered by the Palaeozoic Asturian Massif; in the east, the N/S-trending Rio Miera Flexure forms a structural boundary to the strongly subsiding Basco-Cantabrian Basin. The depositional history of the NCB was strongly influenced by tectonic events which can be related to the evolving Biscay Ocean. These tectoevents give rise to a gross subdivison of the succession into sedimentary megasequences. Three tectonically induced megasequence boundaries can be recognized in the Albian and Cenomanian, defining the Albian and Cenomanian megasequences: • Santander-Tectoevent (Cenomanian/Turonian boundary interval) • Vraconian Tectoevent (late Late Albian) • "Middle Albian event" (break-up unconformity, [?late] Early Albian). The "Middle Albian event" caused a disintegration of the widespread Urgonian Clansay platforms (Late Aptian/Early Albian) into a palaeo-relief of eastward-dipping tilted blocks. In the N/S trending halfgrabens, fluvio-deltaic clastics were deposited during the Middle Albian, whereas the exposed tilted block crests were karstified. A strong transgressive pulse flooded the NCB in the early part of the Late Albian, giving rise to the widespread deposition of marine Upper Albian sediments. This transgressive event can also be recognised in southern Iberia and Portugal. During the later part of the Late Albian, the emergent crestal areas of the tilted blocks were onlapped by marine sediments, resulting in the filling-up of the Middle Albian palaeo-relief. Tectonic movements in the latest Albian (Vraconian tectoevent), causing emergence in wide parts of the NCB, terminated the Albian Megasequence. The Cenomanian megasequence started in the Albian/Cenomanian boundary interval with progradation of deltaic clastics, which were channelized (following the Santi liana-axis) into an eastward direction. This "Santillana Delta" flowed into the Basco-Cantabrian Basin east of Santander, where an interfingering with the prodeltaic sediments of the Valmaseda Delta ("Black Flysch" of the Bilbao area) took place. The differential subsidence in the NCB due to the Vraconian tectoevent was compensated by the deltaic sedimentation. In the lower part of the Mantelliceras mantelli Zone, a transgressive pulse flooded the NCB and led to the deposition of marine, predominantly calcareous sediments. This transgressive event is thought to correlate with the "Early Cenomanian transgression" sensu lato. In the Cenomanian succession of the NCB, the following ammonite zones can be recognized: • Late Cenomanian: Eucalycoceras pentagonum Zone and Metoicoceras geslinianum Zone [pars] • Middle Cenomanian: [Cunningtoniceras inerme Zone], Acanthoceras rhotomagense Zone and A. jukesbrownei Zone • Early Cenomanian: Mantelliceras mantelli Zone and M. dixoni-Zone. The upper part of the Upper Cenomanian (upper part of the geslinianum Zone and the Neocardioceras juddii Zone) is missing in the NCB. In the upper part of the mantelli Zone, deposition of the shallow marine carbonate sediments of the Altamira Platform became established over large areas of the NCB. In the strongly subsiding area east of the Rio Miera Flexure, thick successions of basinal sediments (marls, nodular limestones, marl/limestone rhythmites) were deposited contemporaneously. During the Middle to early Late Cenomanian, the Altamira Platform was drowned in three successive steps from east to west. The developing drowning unconformities (condensed, mineralized hardgrounds with ammonites) young towards the west, resulting in a backstepping of the Altamira Platform. In the Late Cenomanian (pentagonum Zone), all former sites of shallow marine carbonate deposition were drowned. The depositional history of the Cenomanian was terminated in the higher part of the geslinianum Zone when tectonic movements of the Santander tectoevent caused widespread emersion of the NCB. The resulting Cenomanian/Turonian boundary hiatus can be recognized both in the condensation horizons on top of the submerged platform as well as in the basinal successions. The facies development of the Cenomanian Megasequence is dominated by the pulsatory nature of the "Cenomanian transgression". Within the Cenomanian succession of northern Cantabria, six sequence boundaries can be recognized, which define six depositional (3rd-order) sequences (DS Ce I - VI). The stratigraphic positions of the sequence boundaries (SB) are as follows: • SB Ce VI = upper geslinianum Zone • SB Ce V = Middle/Late Cenomanian boundary interval • SB Ce IV = basal jukesbrownei Zone • SB Ce III = upper dixoni Zone • SB Ce II = upper mantelli Zone • SB Ce I = lower mantelli Zone. Comparison of this sequential subdivision with regional cycle charts from the Basco-Cantabrian area reveals good agreement, whereas correlation with the "global sea-level curve" (Exxon Chart) is poor. The extent to which many of the sea-level events in the Cenomanian (e.g. SB Ce III, mfz within the rhotomagense Zone, SB Ce IV, HST in the pentagonum Zone) can be correlated between basins elsewhere in Europe and Tunisia suggests that they were probably of eustatic nature. Considering the Cenomanian Megasequence as a "2nd-order cycle", an overall transgressive trend occurs throughout the Cenomanian; maximum coastal onlap was reached during the maximum flooding of DS Ce VI (pentagonum Zone). Palaeobiogeographically, the NCB shows strong tethyan affinities in the Late Albian and Cenomanian. The Turrilites scheuchzerianus/Neohibolites ultimus event in the early Middle Cenomanian permits a correlation with the Actinocamax primus event of the temperate Cenomanian of northern Europe by means of bio-, sequence and isotope stratigraphy.
    Description: Los sedimentos del Cretácico medio (Albiense superior/Cenomaniense) en la parte septentrional de la Provincia de Cantabria han sido estudiados, centrándose en aspectos estratigráficos y sedimentolögicos. El área de estudio pertenece estructural mente a la Cuenca Norcantábrica (NCB), cuya historia depositional comenzó con movimientos tectónicos distensivos en el Valanginiense medio. La NCB es una de las numerosas cuencas sedimentarias que se desarrollaron en el margen continental norteibérico como consecuencia del "rifting" y apertura del golfo de Vizcaya durante el Mesozoico. Es una cuenca con forma de golfo con una elongatión E/W ("Eje de Santillana"). Los límites septentrional y meridional de la NCB son el "Liencres High" y el Escudo de Cabuemiga respectivamente. Hacia el Oeste, la NCB queda confinada por el Macizo Paleozoico Asturiano; en el Este, el límite estructural conocido como Flexión del Río Miera de dirección N/S, la separa de la Cuenca Vasco-cantábrica mucho más subsidente. La historia deposicional de la NCB estuvo fuertemente influenciada por eventos tectónicos que pueden ser relacionados con la evolution del oceano de Vizcaya. Estos tectoeventos dieron lugar a una gruesa subdivision de la sucesión en megasecuencias sedimentarias. Tres límites de megasecuencias, que están inducidos por la tectónica, pueden ser reconocidos en el Albiense y Cenomaniense, definiendo respectivamente las megasecuencias albienses y cenomanienses: • Tectoevento de Santander (intervalo límite del Cenomaniense/Turoniense) • Tectoevento Vraconiense (Albiense superior tardío) • "Evento del Albiense medio" (discordancia de ruptura, Albiense inferior [?tardio]). El "Evento del Albiense medio" causo una desintegración de las plataformas urgonianas clansayenses (Aptiense superior/Albiense inferior), que estaban muy extendidas en paleorelieves de bloques basculados hacia el Este. Se produjo durante el Albiense medio una sedimentatión clástica fluvio-deltaica en los semi-grabenes, de dirección N/S, mientras que las cimas expuestas de los bloques basculados sufrieron procesos de karstificatión. Un fuerte pulso transgresivo inundó la NCB al comienzo del Albiense superior, dando lugar al depósito de sedimentos marinos en el Albiense superior due alcanzaron una muy amplia extensión. Durante la parte superior del Albiense superior las crestas de los bloques basculados fueron recubiertas por sedimentos marinos, indicando el equilibrio del paleorelieve en el Albiense medio. Los procesos tectónicos al final del Albiense superior (Tectoevento Vraconiense), que causaron la emersión de amplias zonas de la NCB, terminan la megasecuencia albiense. La megasecuencia cenomaniense comenzó en el limite Albiense/Cenomaniense con la progradatión de material clástico deltaico que fue canalizado (siguiendo el Eje de Santillana) hacia el Este. Dicho delta ("Delta de Santillana") discurria al Este de Santander hacia la Cuenca Vasco-cantabrica, interfiriendo con los sedimentos de prodelta del Delta de Valmaseda ("Flysch Negro"). En la parte inferior de la zona de Mantelliceras mantelli, un pulso transgresivo inundó la NCB y permitió el depósito de sedimentos marinos, predominantemente calcáreos. Este evento transgresivo puede ser correlacionado con la "transgresión del Cenomaniense initial" sensu lato. En la sucesion Cenomaniense de la NCB pueden ser reconocidas las siguientes zonas: • Cenomaniense superior: Zona de Eucalycoceras pentagonum y la Zona de Metoicoceras geslinianum [pars] • Cenomaniense medio: [Zona de Cunningtoniceras inerme], Zona de Acanthoceras rhotomagense y Zona de A. jukesbrownei • Cenomaniense inferior: Zona de Mantelliceras mantelli y Zona de M. dixoni. La parte superior del Cenomaniense superior (parte superior de la zona de M. geslinianum y la Zona de Neocardioceras judii) está ausente en la NCB. Los sedimentos marino-someros de naturaleza carbonatada de la "Plataforma de Altamira" comenzaron a depositarse en amplias zonas de la NCB en la parte superior de la zona de mantelli. Al Este de la Flexión de Río Miera, en un área fuertemente subsidente, fueron depositadas contemporáneamente potentes sucesiones de sedimentos de cuenca (margas, calizas nodulares y ritmitas de marga/caliza). Durante el Cenomaniense medio hasta la base del Cenomaniense superior, la Plataforma de Altamira fue inundada desde el Este al Oeste en tres intervalos sucesivos. El desarrollo de discordancias de inundatión ("drowning unconformities" = series condensadas, "hardgrounds" mineralizados con ammonites) resultan más recientes hacia el Oeste, concluyendo en un basculamiento hacia atrás de la Plataforma de Altamira. En el Cenomaniense superior (Zona de pentagonum) todos los anteriores lugares caracterizados por el depósito de carbonates marino-someros fueron anegados. La historia deposicional del Cenomaniense acabó en la parte alta de la zona de geslinianum, cuando movimientos tectonicos del Tectoevento de Santander causaron la emersión generalizada de la NCB. El hiato resultante puede ser reconocido en los horizontes condensados a techo de las plataformas sumergidas e igualmente en las sucesiones de cuenca. El desarrollo de facies del Cenomaniense está dominado por el carácter de pulsos que tuvo la "transgresión cenomaniense". Seis límites de secuencia pueden reconocerse dentro de la sucesión cenomaniense del norte de Cantabria, los cuales definen seis secuencias deposicional es de tercer orden (DS Ce I-VI). La positión estratigráfica de los límites de secuencia (SB) son los siguientes: • SB Ce VI = parte superior de la Zona de geslinianum • SB Ce V = intervalo límite del Cenomaniense medio/superior • SB Ce IV = base de la Zona de jukesbrawnei • SB Ce III = parte superior de la Zona de dixoni • SB Ce II = parte superior de la Zona de mantelli • SB Ce I = parte inferior de la Zona de mantelli. Una comparación de esta subdivisión secuencial con las tablas de ciclos regionales del reino vasco-cantábrico revela una buena correlatión, mientras que la correlatión con la "tabla global" ("Exxon chart") es pobre. La correlatión entre varias cuencas sugiere una causa eustática para los numerosos eventos de cambios del nivel del mar en el Cenomaniense (por ejemplo SB Ce III, mfz dentro de la Zona de rhotomagense, SB Ce IV, HST en la Zona de pentagonum). Considerando la megasecuencia del Cenomaniense como un "ciclo de segundo orden", una tendencia transgresiva general ocurrió a lo largo del Cenomaniense, el máxirno "onlap" costero fue alcanzado durante la máxima inundatión de la DS Ce VI (Zona de pentagonum). Desde el punto de vista paleobiogeográfico, la NCB muestra fuertes afinidades tethyales en el Albiense superior y el Cenomaniense. El "Evento de Turrilites scheuchzerianus/Neohibolites ultimus" al comienzo del Cenomaniense medio permite una correlation con el "Evento de Actinocamax primus" del Cenomaniense de la Provincia templada norteuropea.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Sedimentationsbecken ; Kreide ; Event-Stratigraphie ; Biostratigraphie ; Sequenzstratigraphie ; Albium ; Cenomanium ; Fazies ; Stratigraphie ; Geologische Korrelation ; Paläobiologie ; Paläontologie
    Language: German
    Type: doc-type:book
    Format: 278
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  • 12
    facet.materialart.
    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-05-07
    Description: Die Stammesgeschichte der Ordnung Ptenoglossa (Gastropoda, Caenogastropoda) wird anhand von 179 rezenten und fossilen Arten bis ins Paläozoikum zurückverfolgt. Ihre rezenten Überfamilien, die Cerithiopsoidea, Triphoroidea und Janthinoidea ernähren sich karnivor. Eine kollabral berippte Larvalschale stellt in den rezenten Überfamilien den ursprünglichen Zustand dar und ist die aussagekräftigste schalenmorphologische Symplesiomorphie. Dies erweist sich durch Radulauntersuchungen und den Fossilbericht. Cerithiopsoidea und Triphoroidea fressen Schwämme und bilden gemeinsam mit den mesozoischen Protorculidae ein Monophylum. Die Janthinoidea fressen Coelenteraten. Sie sind nahe mit den mesozoischen Zygopleuridae verwandt. Die Stammlinien der Schwamm- und Coelenteratenfresser waren schon in der Trias getrennt. Die Zygopleuroidea (Zygopleuridae, Pseudozygopleuridae und Protorculidae) sind folglich ein Parataxon. In allen drei Familien der Zygopleuroidea kommt die kollabral berippte Larvalschale vor und repräsentiert den ursprünglichen Zustand. Die paläozoischen Pseudozygopleuridae stellen wahrscheinlich die Schwestergruppe der rezenten und mesozoischen Ptenoglossa dar. Arten der Pseudozygopleuridae mit planktotropher und nicht planktotropher Frühontogenese können biometrisch getrennt werden. Die Abgrenzung nicht planktotropher Pseudozygopleuridae von den devonischen bis karbonischen Palaeozygopleuridae ist schwierig, weil letztere anhand eines nicht planktotrophen Protoconchs definiert wurden. Mit Hilfe von Protoconchvermessungen ist es jedoch meist möglich, beide Gruppen zu trennen. Die Außengruppe der Ptenoglossa sind die Cerithimorpha, die im Paläozoikum durch die Acanthonematidae und die Murchisoniidae repräsentiert werden. Die paläozoischen Acanthonematidae werden neu gefaßt und enthalten nun unter anderem die Gattungen Orthonema, Palaeostylus, Cerithioides und Knightella. Sie zeichnen sich durch einen heliciformen Protoconch aus, der sich grundsätzlich von dem der Pseudozygopleuridae (Ptenoglossa) unterscheidet. Mithin ist der Protoconch der Pseudozygopleuridae die wesentliche schalenmorphologische Apomorphie der Ptenoglossa. 30 Arten werden neu beschrieben (siehe Anhang A), davon 2 rezente, 8 aus dem Tertiär, 1 aus der Kreide, 13 aus der Trias, 1 aus dem Perm und 5 aus dem Karbon. Turritella hybrida MONSTER non DESHAYES erhält den neuen Namen Zygopleura hybridissima nom. nov. 5 neue Gattungen werden errichtet: Antiphora n. Gen. (Triphoroidea, Tertiär), Eorex n. gen. (Triphoroidea, Tertiär), Atorcula n. gen. (Protorculidae, Trias), Azyga n. gen. (Zygopleuridae, Trias) und Stiazyga n. gen. (Zygopleuridae, Trias). Ampezzopleurinae n. subfam. wird als Unterfamilie der Zygopleuridae WENZ errichtet. Nystiellinae CLENCH & TURNER erhält Familienstatus (Nystiellidae). Die Untergattung Cerithiopsis (Vatopsis) GRÜNDEL wird zur Gattung erhoben und von den Cerithiopsidae zu den Eumetulidae transferiert. Tembrockia GRÜNDEL wird von den Cerithiopsidae zu den Eumetulidae transferiert. Variseila DOCKERY wird von den Triforidae JOUSSEAUME zu den Eumetulidae GOLIKOV & STAROBOGATOV transferiert. Ampezzopleura BANDEL wird von den Protorculidae BANDEL zu den Zygopleuridae WENZ transferiert. Zygopleura tenuis (MÜNSTER) sensu Zardini wird als neue nominelle Art Ampezzopleura tenuis BANDEL betrachtet, für die ein Lectotyp hinterlegt wird. Teutonica SCHRÖDER wird von den Cerithiopsidae zu den Zygopleuridae transferiert. Orthonema MEEK & WORTHEN wird von den Turritellidae LOVÉN zu den Acanthonematidae WENZ zurücktransferiert. Palaeostylus MANSUY wird von den Procerithiidae COSSMANN zu den Acanthonematidae transferiert. Knightella LONGSTAFF wird von den Pseudozygopleuridae KNIGHT zu den Acanthonematidae transferiert. Cerithioides HAUGHTON wird von den Murchisoniidae zu den Acanthonematidae WENZ transferiert. Die systematische Stellung einiger weiterer Taxa wird kritisch hinterfragt. Etliche Arten werden anderen Gattungen zugeordnet (siehe Anhang A "comb. nov.").
    Description: The phylogeny of the order Ptenoglossa (Gastropoda, Caenogastropoda) is traced back into the Paleozoic by studying 179 Recent and fossil species. The Recent superfamilies Cerithiopsoidea, Triphoroidea und Janthinoidea are carnivorous. A larval shell with collabral ribs represents the plesiomorphic state in the Recent superfamilies and it is the most informative symplesiomorphy that concerns to the shell morphology. Evidence for that is given by the radula morphology and the fossil record. Cerithiopsoidea and Triphoroidea feed on sponges and form a clade with the Mesozoic family Protorculidae. The Janthinoidea feed on coelenterates. They are closely related to the Mesozoic family Zygopleuridae. The stem lines of sponge eaters and coelenterate eaters have been separated from each other at least since the Triassic. Thus, the superfamily Zygopleuroidea (Zygopleuridae, Pseudozygopleuridae and Protorculidae) is a parataxon. In all three families of the Zygopleuroidea a larval shell with collabral ribs occurs and represents the plesiomorphic state. The Paleozoic Pseudozygopleuridae are presumably the sister-group of the Recent and the Mesozoic Ptenoglossa. Species of the Pseudozygopleuridae with planktotrophic and non-planktotrophic larval development can be separated from each other by measuring their protoconchs. The separation of non-planktotrophic Pseudozygopleuridae from Devonian and Carboniferous species of the Palaeozygopleuridae is difficult because Palaeozygopleuridae were defined by a non-planktotrophic protoconch, whereas Pseudozygopleuridae were defined by a larval shell of the planktotrophic type. But in most cases it is possible to identify the species by protoconch measurements. The outgroup of the Ptenoglossa are the Cerithimorpha which are represented in the Paleozoic by the families Acanthonematidae and Murchisoniidae. The Paleozoic Acanthonematidae are newly defined and contain genera like Orthonema, Palaeostylus, Cerithioides and Knightella. They have a heliciform protoconch which is fundamentally different from the protoconch of the pseudozygopleurids (Ptenoglossa). The protoconch of the Pseudozygopleuridae is the essential apomorphy concerning the shell of the Ptenoglossa. 30 species are described as new (see Anhang A), 2 of which are Recent, 8 are from the Tertiary, 1 from the Cretacous, 13 from the Triassic, 1 from the Permian and 5 from the Carboniferous. Turritella hybrida MÜNSTER non DESHAYES gets the new name Zygopleura hybridissima nom. nov. 5 new genera are erected: Antiphora n. gen. (Triphoroidea, Tertiary), Eorex n. gen. (Triphoroidea, Tertiary), Atorcula n. gen. (Protorculidae, Triassic), Azyga n. gen. (Zygopleuridae, Triassic) and Striazyga n. gen. (Zygopleuridae, Triassic). Ampezzopleurinae n. subfam. is erected as subfamily of the Zygopleuridae. Nystiellinae CLENCH & TURNER is raised on family level (Nystiellidae). The subgenus Cerithiopsis (Vatopsis) GRÜNDEL is raised on genus level and is transferred from Cerithiopsidae H. & A. ADAMS to Eumetulidae GOLIKOV & STAROBOGATOV. Tembrockia GRÜNDEL is transferred from Cerithiopsidae to Eumetulidae. Variseila DOCKERY is transferred from Triforidae JOUSSEAUME to Eumetulidae. Ampezzopleura BANDEL is transferred from Protorculidae BANDEL to Zygopleuridae WENZ. Zygopleura tenuis (MÜNSTER) sensu Zardini is deemed to be the new nominal species Ampezzopleura tenuis BANDEL (type species of Ampezzopleura) for which a lectotype is designated. Teutonica SCHRÖDER is transferred from Cerithiopsidae to Zygopleuridae. Orthonema MEEK & WORTHEN is retransferred from Turritellidae LOVÉN to Acanthonematidae WENZ. Palaeostylus MANSUY is transferred from Procerithiidae COSSMANN to Acanthonematidae. Knightella LONGSTAFF is transferred from Pseudozygopleuridae KNIGHT to Acanthonematidae. Cerithioides HAUGHTON is transferred from Murchisoniidae KOKEN to Acanthonematidae WENZ. The systematic position of several other taxa has been critically revised. The generic position of several species is changed (see Anhang A "comb. nov.").
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläontologie ; Paläobiologie ; Gastropoda
    Language: German
    Type: doc-type:book
    Format: 304
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  • 13
    Publication Date: 2024-05-07
    Description: Die Ordnungen Cerithiimorpha und Littorinimorpha stellen umfangreiche systematische Gruppen innerhalb der basalen Caenogastropoda mit einfachen konisch-orthostrophen Protoconchen dar. Diese Großgruppen lassen sich seit der späten Trias differenzieren und lassen seit der Kreidezeit eine zunehmende Diversität erkennen. Im folgenden werden ausgewählte Vertreter aus fünf Überfamilien und 20 Familien unter besonderer Berücksichtigung ihrer frühontogenetischen Schalen beschrieben und ihre Entwicklungsgeschichte wird seit der Kreide belegt. Die Überfamilie Cerithioidea stellt die Kerngruppe der Cerithiimorpha und war mit der Familie Procerithiidae seit dem Jura weltweit im Flachmarin verbreitet. Form und Skulptur der Larvalschale ermöglichte es, die Gattung Schroederium n.g. von den Gattungen Procerithium und Cryptaulax zu trennen. In der Oberkreide lassen sich die nahe verwandten Familien Cassiopidae, Potamididae, Melanopsidae und Scaliolidae über ihre Protoconchmorphologie sicher von den Procerithiidae differenzieren. Die Familien Batillariidae und Modulidae sind durch ihre charakteristische Embryonalschalenskulptur als Schwestergruppen ausgewiesen. Ihre nahe Verwandtschaft wird auch durch anatomische Daten gestützt. Innerhalb der seit dem Eozän in Protoconcherhaltung dokumentierten Familie Cerithiidae, Unterfamilie Cerithiinae, treten abhängig vom besiedelten Habitat zwei Protoconchtypen auf, die mit zu unterscheidenden Radulatypen korrelieren. Die Unterfamilie Bittiinae konnte über Details der Larvalschalenskulptur seit dem Eozän belegt und von den Cerithiinae differenziert werden. Die Adelphotaxa Planaxidae und Thiaridae mit dem gemeinsamen Merkmal einer Bruttasche im Kopffußbereich sind ebenfalls seit dem Eozän bekannt. Larvalschalen fossiler und rezenter Planaxinae werden vergleichend dargestellt. Larvalschalen der hinsichtlich der Morphologie des Teleoconches abweichenden Unterfamilie Fossarinae belegen die Nähe zur Nominatunterfamilie und ermöglichten eine sichere Abgrenzung von gehäusekonvergenten Vertretern der Littorinimorpha. Über die Formation der frühontogenetischen Schale, die eine charakteristische Embryogenese widerspiegelt, war es möglich, die Brackwasser und limnische Biotope besiedelnden Thiaridae bis in das mittlere Eozän zu belegen, was auch Anlaß zu neuen paläobiogeographischen Interpretationen gab. Pseudamauridae konnten über ihre Protoconche von der Oberkreide bis in das Eozän belegt und von gehäusekonvergenten Naticoidea (Neomesogastropoda) und Amphibolidae innerhalb der Archaeopulmonata (Heterostropha) abgegrenzt werden. Die Phylogenese der Überfamilien Vermetoidea und Turritelloidea wurde von der Unterkreide bis rezent dokumentiert, wobei konvergente Gruppen über ihre Protoconche differenziert wurden. Innerhalb der Littorinimorpha konnten charakteristische Merkmale der Embryonal- und Larvalschalen herausgearbeitet und zur Untergliederung der Littorinoidea und Rissooidea herangezogen werden. Pickworthiidae mit alloisostroph abgewinkelten Protoconchen konnten bis in das Danium belegt werden. Der direkte Vergleich mit Protoconchen der triassischen Protstyliferidae mit detaillierten Übereinstimmungen dokumentiert die unabhängige Evolution dieser Linie. Die konvergenten Vanikoridae ließen sich über ihre Protoconchmorphologie trennen, wobei auch signifikante Unterschiede zu den übrigen Littorinimorpha dargestellt werden. Micromphalina peyrerensis und Megalomphalus (M.) antwerpensis werden neu beschrieben und den Vanikoridae eingegliedert.
    Description: The orders Cerithiimorpha and Littorinimorpha represent large systematic units within the stem of Caenogastropoda with simple conical-orthostrophic protoconchs. These groups are separated since the Upper Triassic showing increasing diversity since the Upper Cretaceous. Representatives of five superfamilies and 20 families are described with special reference to their early ontogenetic shells. The family Procerithiidae within the superfamily Cerithioidea has been distributed worldwide since Jurassic times as a faunal element in shallow marine environments. Regarding the shape and sculpture of its larval shell the procerithiid Schroederium n.g. could be differentiated from the genera Procerithium and Cryptaulax. Since the Upper Cretaceous brackish-water Cassiopidae, Potamididae and Melanopsidae can be differentiated from Procerithiidae by their protoconch-morphology. The families Batillariidae and Modulidae represent Adelphotaxa. This relation is proven by the uniting character of embryonic tuberculated sculpture and data concerning their anatomy. The Cerithiidae, subfamily Cerithiinae, are documented since the Eocene with preserved protoconchs. Two types of larval sculpture are present depending on the settled habitat, correlated with two different types of radulae. The subfamily Bittiinae is also documented and distinguished from the Cerithiinae by their protoconch-morphology since the Eocene. The Adelphotaxa Planaxidae and Thiaridae with the uniting character of a brood pouch within the head-foot are present since the Eocene. Larval shells of fossil and Recent Planaxinae are compared. Protoconchs of representatives of the subfamily Fossarinae with different teleoconch-morphology proved the close relation to the Planaxinae and also made a differentiation from convergent littorinimorphs feasible. The analysis of early ontogenetic shells of brackish water and limnic Thiaridae enabled to trace them back to the Middle Eocene and made new interpretations concerning their palaeobiogeography possible. Pseudamauridae could be documented from the Upper Cretaceous to the Middle Eocene with the aid of preserved protoconchs and could be discriminated from convergent Naticoidea and Archaeopulmonata. The phylogenetic history of Vermetoidea and Turritelloidea could be reconstructed since the Early Cretaceous and convergent groups could be differentiated. Within the Littorinimorpha characters regarding the early shell could be worked out to subdivide Littorinoidea and Rissooidea. Pickworthiidae with alloisostrophic protoconchs are documented since the Danian. Comparison with protoconchs of Triassic Prostyliferidae yielded detailed accordance and documents the independent history of this lineage. The convergent Vanikoridae could be discriminated by their protoconch-morphology and significant differences to the other Littorinimorpha are presented. Micromphalina peyrerensis and Megalomphalus (M.) antwerpensis are described as new species and are included within the Vanikoridae.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Caenogastropoda ; Paläobiologie
    Language: German
    Type: doc-type:book
    Format: 126
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  • 14
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-05-06
    Description: Klaus Bandel & Thorsten Kowalke: Systematic value of the larval shell of fossil and modern Vanikoridae, Pickworthiidae and the genus Fossarus (Caenogastropoda, Mollusca) … 3 ; R. Thomas Becker: Eine neue und älteste Glatziella (Clymeniida) aus dem höheren Oberdevon des Nordsauerlandes (Rheinisches Schiefergebirge) … 31 ; Glenn G. Rechner: Eine Dinoflagellaten-Zysten-Vergesellschaftung des tieferen Rupelium (Unter-Oligozän) aus transgressiven Ablagerungen nördlich von Altenhausen in Sachsen-Anhalt (Blatt 3733, Erxleben) … 43 ; Joachim Gründel: Zur Kenntis einiger Gastropoden-Gattungen aus dem französischen Jura und allgemeine Bemerkungen zur Gastropodenfauna aus dem Dogger Mittel- und Westeuropas … 69 ; Joachim Gründel: Heterostropha (Gastropoda) aus dem Dogger Norddeutschlands und Nordpolens. I. Mathildoidea (Mathildidae) … 131 ; Joachim Gründel: Heterostropha (Gastropoda) aus dem Dogger Norddeutschlands und Nordpolens. III. Opisthobranchia … 177 ; C. M. Hampton & J. E. Rae: Genesis of the fossiliferous Pleistocene Hima Limestone, western Uganda, as indicated by its isotopic composition … 225 ; Helmut Keupp: Anomal kiellose Hildoceratidae (= „Subfamilie Monestierinae SAPUNOV 1965“): Ursache taxonomischer Konfusionen (Ammonoidea, Toarcium) … 233 ; Helmut Keupp: Paläopathologische Analyse einer „Population“ von Dactylioceras athleticum (SIMPSON) aus dem Unter-Toarcium von Schlaifhausen/Oberfranken … 243 ; Rolf Kohring: Eischalen neognather Vögel aus dem mitteleozänen Geiseltal (Deutschland) … 269 ; Rolf Kohring: Eggshell Structure as Evidence in Avian Systematics - Preliminary Results … 281 ; Jürgen Kriwet: Beitrag zur Kenntnis der Fischfauna des Oberjura (unteres Kimmeridgium) der Kohlengrube Guimarota bei Leiria, Mittel-Portugal: 2. Neoselachii (Pisces, Elasmobranchii) ... 293 ; Thomas Schlüter: Validity of the Paratrichoptera - an extinct Insect Order related to the Mecoptera, Diptera, Trichoptera or Lepidoptera? Suggestions based on discoveries in the Upper Triassic Molteno Formation of South Africa … 303 ; Rolf Kohring: Bibliographie 1996, Institut für Paläontologie, Freie Universität Berlin … 313 ;
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläobiologie ; Paläontologie
    Language: German , English
    Type: doc-type:book
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  • 15
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: Contents ; List of Contributors ; Introduction ; I. General Problems of Sponge Biology. S. M. Efremova: Once more on the position among Metazoa - Gastrulation and germinal layers of sponges ; N. N. Marfenin: Sponges viewed in the light of up-to-date conception on coloniality ; A. V. Ereskovsky & G. P. Korotkova: The reasons of sponge sexual morphogenesis peculiarities II. Developmental Biology of Sponges. O. M. Ivanova-Kazas: Analysis of the sponges ontogeny at sexual reproduction ; R. P. Anakina: The cleavage specifity in embryos of the Barents Sea sponge Leucosolenia complicata Montagu (Calcispongiae, Calcaronea) ; L. V. Ivanova: New data about morphology and metamorphosis of the spongillid larvae (Porifera, Spongillidae). 1. Morphology of the free-swimming larvae ; L. V. Ivanova: New data about morphology and metamorphosis of the spongillid larvae (Porifera, Spongillidae). 2. The metamorphosis of the spongillid larvae ; L. V. Ivanova & V. V. Semenov: Feeding habits of the larvae of sponges ; N. A. Sizova & A. V. Ereskovsky: Ultrastructural peculiarities of the early embryogenesis in a White Sea sponge Halisarca dujardini (Demospongiae, Dendroceratida) ; III. Ecology of Sponges. R. P. Anakina & E. I. Slepian: Spiculas' malformations of freshwater sponges as indicators of water environment in St. Petersburg City ; A. S. Plotkin & A. V. Ereskovsky: Ecological aspects of asexual reproduction of the White Sea sponge Polymastia mammillaris (Demospongiae, Tetractinomorpha) in Kandalaksha Bay ; I. S. Smirnov & V. M. Koltun: Symbiosis of the antarctic sponge genus lophon (Porifera) and ophiuroid genus Ophiurolepis (Ophiuroidea, Echinodermata) ; IV. Palaeontology and Systematics. L. V. Bolshakova: Stromatoporoids - the fossil sponges ; E. V. Veinberg, 0. M. Khlystov, S. S. Vorobyova, E. G. Kornakova, 0. V. Levina, S. M. Efremova, & M. A. Grachev: Distribution of sponge spicules in sediments of the underwater Akademichesky ridge of Lake Baikal ; K. R. Tabachnik & C. Levi: Amphidiscophoran Hexasterophora (Part I & II) ;
    Description: conference
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Porifera ; Paläobiologie
    Language: English
    Type: doc-type:book
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  • 16
    facet.materialart.
    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: At the beginning of Late Jurassic both the Lochen (LA) and the Cracow areas (CA) were palaeotopographic highs in an epicontinental basin located at the stable northern margin of the Tethyan Ocean. The topographically high position of the LA was probably caused by intensive carbonate production which proceeded on a small sea-floor bulge located close to the boundary between middle and lower parts of the low-angle carbonate ramp. Lack of deep structural control of this rise caused prograding facial unification during the Oxfordian and Kimmeridgian and led to gradual disappearance of the LA individuality in relation to the neighbouring areas. The topographical high of the CA resulted from anomalously low subsidence rate in comparison to the adjacent areas which has lasted at least for the whole Oxfordian. Low subsidence directly gave rise to the development of a barrier (so-called Cracovian Platform) which separated the interior basin in the north from the deeper parts of the basin in the south. Topography of the Polish part of epicontinental basin along the Czestochowa-Cracow line corresponds to the low-gradient rimmed carbonate shelf which graded laterally (to the northeast and east) into the low-angle carbonate ramp. Stratigraphic subdivision of Upper Jurassic strata is very precise in the LA and rather poor in the CA due to scarcity of ammonites in the massive facies which predominates in the latter area. However, ammonite fauna from both areas belongs to the same German-Polish Submediterranean Subprovince which allows to attempt the correlation of lithologies and determination of factors which controlled deposition. Both the studied areas show distinct differences in the development of carbonate buildups. In the LA the main components of carbonate buildups during whole Oxfordian and the Early Kimmeridgian were siliceous sponges and microbolites whilst in the CA the flourishing growth of microbolites and gradual decline of siliceous sponges domination took place during the Late Oxfordian. The sediment was initially diversified into the two varieties: that formed by siliceous sponges and the microbolites incipient rigid framework, and the soft mud. In such carbonate buildups stromatactis cavities might have developed even in early diagenesis due to internal erosion of the soft mud. The principal reason of the internal erosion was turbulent water flow through the sediment. However, in generally low-energy sedimentary environments such flow could be triggered by submarine gravity flows or strong bottom currents. Pseudonodular textures encountered in carbonate buildups in both the areas resulted from shallow-burial diagenesis. During the burial diagenesis some parts of the sediment has been disintegrated under the pressure of overlying strata owing to the existing open spaces and different susceptibility to compaction showed by the incipient rigid framework and the soft sediment. Deposition in the LA was controlled mainly by sea-level pulses and ecological factors. In the CA principal control was provided by subsidence rate supported by synsedimentary tectonics, sea-level changes and ecological factors. All these controlling factors were variable in time which provoked changes in carbonate production rates from intensive, aggradational growth of the buildups to drowning of the carbonate ramp and rimmed shelf. The drowning of carbonate ramp on which the LA was located took place at the Oxfordian/Kimmeridgian break. It is documented by spectacular development of redeposited pelagites of skeletal-calciturbidites type with abundant fragments of Saccocoma sp. which have appeared for the first time in mass quantities in the Upper Jurassic. By analogy, it can be inferred that in the CA similar Saccocoma-calciturbidites prove the drowning of rimmed shelf related to the same trangressive event at the Oxfordian/Kimmeridgian break.
    Description: Zu Beginn des Ober-Jura waren das Lochengebiet (Schwäbische Alb) und der Raum Krakau (Südpolen) übereinstimmend Hochgebiete eines epikontinentalen Beckens auf dem passiven nördlichen Schelf der Tethys. Die topographische Hochposition des Lochengebietes war vermutlich durch eine hohe Karbonat-Produktion bedingt, welche auf einer schmalen submarinen Schwelle nahe dem Übergangsbereich zwischen unterem und mittlerem Abschnitt einer flach geneigten Karbonatrampe erfolgte. Während des Oxfordiums und Kimmeridgiums war die Lochenschwelle tektonisch inaktiv und ermöglichte einen zunehmenden Faziesausgleich mit den benachbarten Gebieten und führte dadurch zu einer successiven Aufgabe ihrer individuellen Entwicklung. Die Hochposition der Krakau-Region resultierte aus ihrer im Vergleich zur Umgebung ungewöhnlich geringen Subsidenzrate, welche mindestens während des gesamten Oxfordiums anhielt. Die geringe Subsidenz war unmittelbare Ursache für die Entwicklung einer Barriere (die sogenannte Krakau-Plattform), welche das seichtere Innenschelf-Becken im Norden von den tieferen Beckenanteilen im Süden trennte. Die Topographie des polnischen Anteils dieses epikontinentalen Beckens entsprach entlang der Czestochowa-Krakau-Linie einem „low-gradient rimmed carbonate shelf, der nach Nordosten und Osten lateral in eine flache Karbonatrampe überging. Die stratigraphische Gliederungsmöglichkeit der Ober-Jura-Schichfolge ist im Lochengebiet gut und feinauflösend, in der Krakau-Region dagegen, in der die Massenfazies vorherrscht, aufgrund der selteneren Ammonitenfunde zum Teil problematisch. Ungeachtet dessen, gehören die Ammoniten-Vergesellschaftungen beider Regionen derselben deutsch-polnischen, submediterranen Faunensubprovinz an und ermutigen zu einer Korrelation beider lithologischer Abfolgen und einer vergleichenden Abstraktion der Steuermechanismen für die Sedimentation. Beide Gebiete zeigen deutliche Unterschiede in der Entwicklung von karbonatischen Buildups. Im Lochen-Gebiet stellen während des Oxfordiums und Unter-Kimmeridgiums Kieselschwämme und Mikrobolithe die Hauptkomponenten der Riffstrukturen, während in der Krakau-Region die Bedeutung der Mikrobolithe und Kieselschwämme während des Ober-Oxfordiums successive abnimmt. Ursprünglich erfolgte eine Differenzierung der Riffstrukturen in einen autochthonen Hartsubstrat-Anteil, in dem Kieselschwämme und Mikrobolithe eine rigides Gerüst stellten, und in schlammiges Weichsubstrat. Innerhalb der Riffkörper konnten sich wohl frühdiagenetisch durch die interne Erosion der Schlamm-Anteile Stromatactis-Gefüge bilden. Grundsätzlich kann eine solche interne Erosion auf turbulente Porenwasserströme zurückgeführt werden. In den vorliegenden sedimentären Stillwasser-Milieus könnte ein solcher Porenwasserstrom durch submarine Schuttströme oder starke Bodenströmungen ausgelöst worden sein. Pseudonodulare Strukturen, wie sie in den Buildups beider Untersuchungsgebiete angetroffen wurden, werden durch eine flache Versenkungsdiagenese erklärt. Während dieser Vorgänge wurden unter dem Druck der Sedimentauflast aufgrund des vorhandenen, offenen Porenraumes und der unterschiedlichen Kompaktion von primär zementierten Riffkalken und des mergeligen Weichsubstrates Karbonatanteile gelöst. Das Sedimentationsgeschehen wurde in der Lochen-Region vor allem durch Meeresspiegel-Schwankungen und ökologische Parameter beeinflußt. In der Krakau-Region konnte als hauptsächlicher Kontrollfaktor die Subsidenzrate erkannt werden, in deren Gefolge synsedimentäre Tektonik, Änderungen von Meeresspiegel und der ökologischen Faktoren einhergingen. Veränderungen dieser Steuerfaktoren in der Zeit beeinflußten jeweils die Rate der Karbonatproduktion von intensiv (Aggradation der Buildups) bis zum Ertrinken der Karbonatrampe bzw. des Schelfrandes. Das Abtauchen der Karbonatrampe setzte in der Lochen-Region an der Oxfordium-Kimmeridgium-Wende ein. Es wird durch eine auffällige sedimentäre Entwicklung dokumentiert: Resedimentation pelagischer Kalke (skeletal calciturbidites), die häufig Saccocoma-Reste enthalten. Erste Massenvorkommen von Saccocoma treten in der Erdgeschichte im Oberjura auf. Ähnliche Saccoco/na-Kalkturbidite an der Oxfordium-Kimmeridgium-Grenze markieren in der Krakau-Region das Abtauchen des „rimmed shelf. Sie können auf dasselbe transgressive Ereignis zurückgeführt werden.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; ddc:554 ; Paläobiologie
    Language: English
    Type: doc-type:book
    Format: 116
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  • 17
    Publication Date: 2024-04-17
    Description: The present study considered calcareous nannofossils from material represented by outcrops of Flysch successions of the External Hellenides belt in the area of the Ionian Zone (I.Z.), northwestern Greece. The studied outcrops are located in Epirus mainland and the Ionian island Korfu. Three subdivisions have been traditionally in literature distinguished in the I.Z., the Internal, Middle and External (moving from east to the west), each of which was subsequently recognized in the Flysch deposits as well. Aim of the study was, a refinement of the current biostratigraphic resolution of the area through detailed taxonomic descriptions and consequently, a reliably better correlation of the investigated sedimentary deposits with the help of calcareous nannofossils. The biostratigraphic data were also processed semiquentitatively (frequency variations and distributions), in order to accurately determine important biohorizons. For this purpose, the nannofossils were studied under the LM and the SEM, from ten closely sampled sections representing clastic sequences of all the three subdivisions of the I.Z. The investigated sections are situated at about 39° northern mid latitudes, a fact which resulted to mixed nannoflora assemblages of low and high latitudes character. The sections are namely: Elatos, Korfovouni (Internal I.Z. subdivision), Kato Despotiko, Strouga Goumenou and Ekklisia (Middle I.Z. subdivision), lower and upper Argyrotopos, National Road, Monos and Anacharavi (External I.Z. subdivision). They were found to range in age from the latest Eocene to the Early Miocene. Based on the systematic palaeontology, 107 species of calcareous nannofossils were observed and documented in the studied material. Among them, a new species Rhabdosphaera epirotica sp. nov. was described, and four recombinations were proposed. Moreover, two calcareous dinoflagellate cysts, Cervisiella saxea and Obliquipithonella sp. were reported for the first time from the I.Z. in Greece. Despite the mid latitude palaeogeographic position of the sections, all the conventional calcareous nannofossil zonal markers for the Oligocene and Early Miocene were recorded, although some in fewer abundances than in low latitudes. Improving the biostratigraphic reliability, a new zonational scheme was here developed and proposed for the Oligocene to Early Miocene interval. It was mainly established on use of redefined biohorizons and composed of five zones and five subzones following below: 1. Latest Eocene: Ericsonia formosa Partial-range Zone, 2. Oligocene: llselithina fusa / Ericsonia formosa Concurrent-range Zone, Ericsonia formosa-Reticulofenestra umbilicus/R. hillae Interval Zone, Cyclicargolithus abisectus Partial-range Zone, including the subzones: Rhabdosphaera spp. Interval Subzone, and Sphenolithus predistentus Interval Subzone, Reticulofenestra scissura Interval Zone, including the Sphenolithus delphix Abundance Subzone, and 3. Earliest Miocene: Triquetrorhabdulus spp. Partial-range Subzone Sphenolithus conicus Interval Subzone. Based on a new biohorizon of the absolute First Occurrence (FO) of llselithina fusa, the Eocene/Oligocene (E/O) boundary was identified in the lower part of the Argyrotopos section. On the absence of disc-shaped discoasters, the I. fusa biohorizon represented a better approximation of the boundary, which was clearly correlated with the other studied sections of the three subdivisions of the I.Z. The Oligocene/Miocene (O/M) boundary was identified in the Monos section located in the Plataria syncline (External I.Z.), but Early Miocene strata were recorded in the Middle I.Z. as well. This boundary was placed at the Last Common Occurrence (LCO) biohorizon of the Reticulofenestra scissura. Moreover, six associate bioevents were reported near the O/M boundary, among them the highest occurrence of I. fusa, located above the boundary, in the Anacharavi section of Korfu island (western part of the External I.Z.). For the first time were evaluated reworked together with „autochton“ taxa of calcareous nannofossils in Greece. Maximum diversity values along each of the studied sections, have shown increased reworking and erosional processes in the Internal subdivision of the I.Z. than in the Middle and the External ones. This is interpreted to be connected with the higher tectonic instability along the Pindos thrust to the east, in relation to the central and western parts of the Ionian basin mainly during the Oligocene.
    Description: Die der vorliegenden Arbeit zugrundeliegenden kalkigen Nannofossilien stammen von Flyschabfolgen der Externen Helleniden (Ionische Zone) Nordwest-Griechenlands.So wurden in die Untersuchung Aufschlüsse des Festlandes in Epirus und der Ionischen Insel Korfu aus dem stratigraphischen Intervall vom obersten Eozän bis zum untersten Miozän einbezogen. Die Ionische Zone (I.Z.) wird traditionell von Osten nach Westen in die Interne, Mittlere und Externe Subzone unterteilt. Diese Einteilung läßt sich auch auf die Flyschablagerungen übertragen. Ziel der Arbeit ist eine Verfeinerung der bestehenden Biostratigraphie durch detaillierte taxonomische Beschreibungen, um damit eine bessere Korrelation der untersuchten Ablagerungen mit Hilfe der kalkigen Nannofossilien zu erreichen. Mit einer halbquantitativen Erfassung der biostratigraphischen Daten (Häufigkeitsvariation und -Verteilung) gelingt es darüberhinaus, einzelne Biohorizonte genauer zu definieren. Zu diesem Zwecke wurde das kalkige Nannoplankton von zehn eng-beprobten Profilen aus klastischen Abfolgen aller drei Subzonen der I. Z. unter dem Licht- und Elektronenmikroskop (REM) untersucht. Die Profile im einzelnen sind: Elatos und Korfovouni (Interne Subzone), Kato Despotiko, Strouga Goumenou und Ekklisia (Mittlere Subzone), Unter bzw. Ober Argyrotopos, National Road, Monos und Anacharavi (Externe Subzone). Zur Ablagerungszeit befanden sich die untersuchten Profile in einer nördlichen Paläobreite um 39°, was zu einer gemischten Nannoflora aus charakteristischen Vertretern niedriger und höherer Breiten führte. In dem untersuchten Material konnten insgesamt 107 Spezies von kalkigem Nannoplankton gefunden und dokumentiert werden. Die Art Rhabdosphaera epirotica nov. sp.wird neu beschrieben und vier Rekombinationen werden vorgeschlagen. Darüberhinaus konnten zwei kalkige Dinoflagellatenzysten Cervisiella saxea und Obliquipithonella sp. zum ersten Mal in der I.Z. nachgewiesen werden. Trotz der paläogeographischen Position der Profile in mittleren Paläobreitenbereich konnten alle konventionellen Zonenleitformen des kalkigen Nannoplanktons für das Oligozän und das Untermiozän gefunden werden, einige davon jedoch in geringerer Häufigkeit als in den niedrigeren Breiten. Durch die Verbesserung der biostratigraphischen Genauigkeit wird hier ein neues mediterranes Zonenschema für das Oligozän und das Untermiozän entwickelt, das im wesentlichen auf neu definierten Biohorizonten basiert. Es enthält fünf Zonen und fünf Subzonen: 1. Jüngstes Eozän: Ericsonia formosa Partial-range Zone, 2. Oligozän: llselithina fusa/Ericsonia formosa Concurrent-range Zone, Ericsonia formosa-Reticulofenestra umbilicus/R. hillae Interval Zone, Cyclicargolithus abisectus Partial-range Zone, gegliedert in den Subzonen: Rhabdosphaera spp. Interval Subzone, und Sphenolithus predistentus Interval Subzone, Reticulofenestra scissura Interval Zone, die eine Subzone enthält: Sphenolithus delphix Abundance Subzone, und 3. Ältestes Miozän: Triquetrorhabdulus spp. Partial-range Subzone Sphenolithus conicus Interval Subzone. Mit dem ersten Auftreten (FO) von llselithina fusa wird ein neuer Biohorizont definiert, mit dem die Grenze Eozän/Oligozän (E/O) in dem unteren Teil des Argyrotopos-Profils nachgewiesen wird. Trotz der Abwesenheit von scheibenförmigen Discoasteriden läßt sich nun diese Grenze mit dem I. fusa-Biohorizont besser fassen und kann eindeutig mit den Profilen in den beiden anderen Subzonen der I.Z. korreliert werden. Die Oligozän/Miozän-Grenze (O/M) konnte im Monos-Profil der Plataria-Synklinale (Externe I.Z.) charakterisiert werden. Untermiozän ließ sich aber auch in der Mittleren Subzone nachweisen. Die Grenze O/M ist durch das letzte Vorkommen (LCO) von Reticulofenestra scissura bestimmt. Sechs assoziierte Bioevents fallen in diesen Grenzbereich, darunter im Anacharavi-Profil der Insel Korfu (Westteil der Externen Subzone) das jüngste Vorkommen von I. fusa, unmittelbar über der Grenze O/M. Zum erstem Mal für Griechenland konnten aufgearbeitete Taxa von kalkigen Nannofossilien zusammen mit den autochthonen Taxa nachgewiesen werden. Ein Vergleich der maximalen Diversitätswerte in den untersuchten Profilen zeigt eine signifikant höhere Aufarbeitungsrate in der Internen Subzone gegenüber der Mittleren und Externen Subzonen. Dieser Umstand dürfte mit der höheren tektonischen Instabilität entlang der Pindos-Decken-Front im Osten des Arbeitsgebietes Zusammenhängen.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Tertiär ; Flysch ; Nannofossil ; Biostratigraphie ; Systematik ; Paläobiologie ; Paläontologie
    Language: English
    Type: doc-type:book
    Format: 206
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