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  • 1
    Keywords: Unterkarbon ; Unteres Karbon ; Carboniferous ; Estratigrafia ; Europe ; Geology ; Geology, Stratigraphic ; Mississippian ; New Mexico
    Description / Table of Contents: Peter Strogen, Ian D. Somerville, and Gareth Ll. Jones: Preface / Geological Society, London, Special Publications, 107:vii-ix, doi:10.1144/GSL.SP.1996.107.01.01 --- Mineralization, Hydrocarbons and Diagenesis --- J. D. Johnston, D. Coller, G. Millar, and M. F. Critchley: Basement structural controls on Carboniferous-hosted base metal mineral deposits in Ireland / Geological Society, London, Special Publications, 107:1-21, doi:10.1144/GSL.SP.1996.107.01.02 --- E. Shearley, P. Redmond, M. King, and R. Goodman: Geological controls on mineralization and dolomitization of the Lisheen Zn-Pb-Ag deposit, Co. Tipperary, Ireland / Geological Society, London, Special Publications, 107:23-33, doi:10.1144/GSL.SP.1996.107.01.03 --- Cathy Hollis, Gordon Walkden, and Cathy Hollis: The use of burial diagenetic calcite cements to determine the controls upon hydrocarbon emplacement and mineralization on a carbonate platform, Derbyshire, England / Geological Society, London, Special Publications, 107:35-49, doi:10.1144/GSL.SP.1996.107.01.04 --- C. Veale and J. Parnell: Metal-organic interactions in the Dinantian Solway Basin, UK: inferences for oil migration studies / Geological Society, London, Special Publications, 107:51-63, doi:10.1144/GSL.SP.1996.107.01.05 --- Carbonate Buildups and Waulsortian Mud-Mounds --- Neil A. H. Pickard: Evidence for microbial influence on the development of Lower Carboniferous buildups / Geological Society, London, Special Publications, 107:65-82, doi:10.1144/GSL.SP.1996.107.01.06 --- Wayne M. Ahr and Robert J. Stanton, Jr.: Constituent composition of Early Mississippian carbonate buildups and their level-bottom equivalents, Sacramento Mountains, New Mexico / Geological Society, London, Special Publications, 107:83-95, doi:10.1144/GSL.SP.1996.107.01.07 --- Kent C. Kirkby and Dave Hunt: Episodic growth of a Waulsortian buildup: the Lower Carboniferous Muleshoe Mound, Sacramento Mountains, New Mexico, USA / Geological Society, London, Special Publications, 107:97-110, doi:10.1144/GSL.SP.1996.107.01.08 --- David L. Jeffery and Robert J. Stanton, Jr.: Biotic gradients on a homoclinal ramp: the Alamogordo Member of the Lake Valley Formation, Lower Mississippian, New Mexico, USA / Geological Society, London, Special Publications, 107:111-126, doi:10.1144/GSL.SP.1996.107.01.09 --- Ian D. Somerville, Peter Strogen, Gareth LL. Jones, and H. E. Anne Somerville: Late Viséan buildups at Kingscourt, Ireland: possible precursors for Upper Carboniferous bioherms / Geological Society, London, Special Publications, 107:127-144, doi:10.1144/GSL.SP.1996.107.01.10 --- Sergio Rodríguez: Development of coral reef-facies during the Viséan at Los Santos de Maimona, SW Spain / Geological Society, London, Special Publications, 107:145-152, doi:10.1144/GSL.SP.1996.107.01.11 --- Siliciclastic Rocks --- Carmen Moreno, Sonia Sierra, and Reinaldo Sáez: Evidence for catastrophism at the Famennian-Dinantian boundary in the Iberian Pyrite Belt / Geological Society, London, Special Publications, 107:153-162, doi:10.1144/GSL.SP.1996.107.01.12 --- Kelly Maguire, Jillian Thompson, and Stuart Gowland: Dinantian depositional environments along the northern margin of the Solway Basin, UK / Geological Society, London, Special Publications, 107:163-182, doi:10.1144/GSL.SP.1996.107.01.13 --- John R. Graham: Dinantian river systems and coastal zone sedimentation in northwest Ireland / Geological Society, London, Special Publications, 107:183-206, doi:10.1144/GSL.SP.1996.107.01.14 --- Carbonate Platforms and Ramps --- Giancarlo Rizzi, Colin J. R. Braithwaite, and Giancarlo Rizzi: Cyclic emersion surfaces and channels within Dinantian limestones hosting the giant Navan Zn-Pb deposit, Ireland / Geological Society, London, Special Publications, 107:207-219, doi:10.1144/GSL.SP.1996.107.01.15 --- A. D. Horbury and A. E. Adams: Microfacies associations in Asbian carbonates: an example from the Urswick Limestone Formation of the southern Lake District, northern England / Geological Society, London, Special Publications, 107:221-237, doi:10.1144/GSL.SP.1996.107.01.16 --- Stephen J. Gallagher: The stratigraphy and cyclicity of the late Dinantian platform carbonates in parts of southern and western Ireland / Geological Society, London, Special Publications, 107:239-251, doi:10.1144/GSL.SP.1996.107.01.17 --- John G. Kelly: Initiation, growth and decline of a tectonically controlled Asbian carbonate ramp: Cuilcagh Mountain area, NW Ireland / Geological Society, London, Special Publications, 107:253-262, doi:10.1144/GSL.SP.1996.107.01.18 --- P. Strogen, I. D. Somerville, N. A. H. Pickard, G. LL. Jones, and M. Fleming: Controls on ramp, platform and basinal sedimentation in the Dinantian of the Dublin Basin and Shannon Trough, Ireland / Geological Society, London, Special Publications, 107:263-279, doi:10.1144/GSL.SP.1996.107.01.19 --- Simon Vanstone: The influence of climatic change on exposure surface development: a case study from the Late Dinantian of England and Wales / Geological Society, London, Special Publications, 107:281-301, doi:10.1144/GSL.SP.1996.107.01.20 --- Basinal Facies --- Hans-Jürgen Gursky: Siliceous rocks of the Culm Basin, Germany / Geological Society, London, Special Publications, 107:303-314, doi:10.1144/GSL.SP.1996.107.01.21 --- Zdzislaw Belka, Stanislaw Skompski, and Janina Sobon-Podgorska: Reconstruction of a lost carbonate platform on the shelf of Fennosarmatia: evidence from Viséan polymictic debrites, Holy Cross Mountains, Poland / Geological Society, London, Special Publications, 107:315-329, doi:10.1144/GSL.SP.1996.107.01.22 --- D. Naylor, G. D. Sevastopulo, and A. G. Sleeman: Contemporaneous erosion and reworking within the Dinantian of the South Munster Basin / Geological Society, London, Special Publications, 107:331-343, doi:10.1144/GSL.SP.1996.107.01.23 --- J. G. Rees, J. D. Cornwell, Z. K. Dabek, and R. J. Merriman: The Apedale tuffs, North Staffordshire: probable remnants of a late Asbian/Brigantian (P1a) volcanic centre / Geological Society, London, Special Publications, 107:345-357, doi:10.1144/GSL.SP.1996.107.01.24 --- Faunas, Floras and Biostratigraphy --- Mariya KH. Makhlina: Cyclic stratigraphy, facies and fauna of the Lower Carboniferous (Dinantian) of the Moscow Syneclise and Voronezh Anteclise / Geological Society, London, Special Publications, 107:359-364, doi:10.1144/GSL.SP.1996.107.01.25 --- G. A. Rukina: Sequence biostratigraphy of the Tournaisian-Lower Viséan rocks of the Russian Platform / Geological Society, London, Special Publications, 107:365-369, doi:10.1144/GSL.SP.1996.107.01.26 --- G. LL. Jones and I. D. Somerville: Irish Dinantian biostratigraphy: practical applications / Geological Society, London, Special Publications, 107:371-385, doi:10.1144/GSL.SP.1996.107.01.27 --- O. A. Lebedev: Fish assemblages in the Tournaisian-Viséan environments of the East European Platform / Geological Society, London, Special Publications, 107:387-415, doi:10.1144/GSL.SP.1996.107.01.28 --- A. Ivanov: The Early Carboniferous chondrichthyans of the South Urals, Russia / Geological Society, London, Special Publications, 107:417-425, doi:10.1144/GSL.SP.1996.107.01.29 --- David A. T. Harper and Anna L. Jeffrey: Mid-Dinantian brachiopod biofacies from western Ireland / Geological Society, London, Special Publications, 107:427-436, doi:10.1144/GSL.SP.1996.107.01.30 --- Jim Smith: A palynofacies analysis of the Dinantian (Asbian) Glenade Sandstone Formation of the Leitrim Group, northwest Ireland / Geological Society, London, Special Publications, 107:437-448, doi:10.1144/GSL.SP.1996.107.01.31
    Pages: Online-Ressource (IX, 463 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799586
    Language: English
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  • 2
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The Wexford Basin (south-eastern Ireland) is a NE–SW-trending sedimentary basin containing carbonates and evaporites deposited during the Late Tournaisian and Viséan. Two separate depositional areas are defined on the basis of facies and facies associations. Sediments were deposited in inner ramp, lagoonal and peritidal environments near Rosslare, and in a more open-marine, shallow- to moderately deep-water, mid to outer ramp environment in the western area around Duncormick. Thick breccia deposits that occur in the Wexford Basin formed as a result of (i) fault movement that produced syn-sedimentary debris flows in the Late? Chadian (Breccia type I); (ii) dissolution of anhydrite/gypsum and subsequent collapse of sedimentary strata (Breccia type II); and (iii) fracturing and brecciation of porous rock caused by the movement of high temperature, late diagenetic fluids along fault planes (Breccia type III). The NE–SW facies polarity displayed by both sedimentary successions was the result of NW–SE extension and the reactivation of the NE–SW-trending Wexford Boundary Fault during the Chadian. Extension at the SE margin of the basin with downthrow to the NNW gave the basin a half-graben character. Thickening of the debris flow deposits to the SW suggests that while the half-graben was being tilted it also underwent a NE–SW block rotation due to an axial component of that normal fault.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The Waulsortian Limestone (Lower Carboniferous) of the southern Irish Midlands is dolomitized pervasively over a much larger region than previous studies have documented. This study indicates a complex, multistage, multiple fluid history for regional dolomitization. Partially and completely dolomitized sections of Waulsortian Limestones are characterized by finely crystalline (0·01–0·3 mm) planar dolomite. Planar replacive dolomite is commonly followed by coarse (≥0·5 mm) nonplanar replacive dolomite, and pervasive void-filling saddle dolomite cement is frequently associated with Zn–Pb mineralization. Planar dolomite has average δ18O and δ13C values (‰ PDB) of –4·8 and 3·9 respectively. These are lower oxygen and slightly higher carbon isotope values than averages for marine limestones in the Waulsortian (δ18O=–2·2, δ13C=3·7). Mean C and O isotope values of planar replacive dolomite are also distinct from those of nonplanar and saddle dolomite cement (–7·0 and 3·3; –7·4 and 2·4 respectively). Fluid inclusions indicate a complex history involving at least three chemically and thermally distinct fluids during dolomite cementation. The petrography and geochemistry of planar dolomites are consistent with an early diagenetic origin, possibly in equilibrium with modified Carboniferous sea water. Where the Waulsortian was exposed to hydrothermal fluids (70–280 °C), planar dolomite underwent a neomorphic recrystallization to a coarser crystalline, planar and nonplanar dolomite characterized by lower δ18O values. Void-filling dolomite cement is isotopically similar to nonplanar, replacive dolomite and reflects a similar origin from hydrothermal fluids. This history of multiple stages of dolomitization is significantly more complex than earlier models proposed for the Irish Midlands and provides a framework upon which to test competing models of regional vs. localized fluid flow.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 1992-04-01
    Print ISSN: 0072-1050
    Electronic ISSN: 1099-1034
    Topics: Geosciences
    Published by Wiley
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  • 5
    Publication Date: 2011-11-01
    Description: The Carboniferous succession in Adarouch (Central Morocco, north of the Atlas Transform Fault) contains thick carbonate beds including upper Visean, Serpukhovian and basal Bashkirian rocks. Foraminifers enable precise recognition of the Visean/Serpukhovian (V/S), early/late Serpukhovian (eS/lS) and Serpukhovian/Bashkirian (S/B) boundaries. Insolentitheca horrida, Loeblichia ukrainica, "Millerella" spp. and Endostaffella? sp. 2 are regarded as regionally useful indices to the V/S boundary, whereas Eostaffellina spp., Eostaffella pseudostruvei and some evolved species of Archaediscus exhibit greater reliability for worldwide correlation of this level. Similarly, the eS/lS boundary is marked locally by Brenckleina rugosa, Eosigmoilina sp., and Monotaxinoides spp. and globally by Loeblichia minima, Bradyina cribrostomata, Plectostaffella spp., Eostaffellina "protvae" and "Turrispiroides", and the S/B boundary is marked locally by Globivalulina bulloides and globally by Seminovella elegantula, and Novella?. Occurrences of these taxa in Morocco allow correlations with the Moscow Basin, the Urals, the Donetz Basin and North America. The Moroccan assemblages share few taxa in common with Saharan basins south of the Atlas Transform Fault. Correlations with western European basins are difficult because of the paucity in the latter of foraminiferal-bearing carbonate strata.
    Print ISSN: 0022-3360
    Electronic ISSN: 1937-2337
    Topics: Geosciences
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  • 6
    Publication Date: 2018-12-01
    Print ISSN: 2095-9273
    Electronic ISSN: 2095-9281
    Topics: Natural Sciences in General
    Published by Elsevier
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  • 7
    Publication Date: 2014-09-26
    Print ISSN: 0078-0421
    Electronic ISSN: 0078-0421
    Topics: Geosciences
    Published by Schweizerbart
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  • 8
    Publication Date: 2003-01-01
    Print ISSN: 0172-9179
    Electronic ISSN: 1612-4820
    Topics: Geography , Geosciences
    Published by Springer
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