ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

X
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Monograph available for loan
    Monograph available for loan
    Petroleum Geology of the Black Sea (2018)
    London : The Geological Society
    Associated volumes
    Details Availability
    Call number: 9/M 07.0421(464)
    In: Geological Society Special Publication
    Description / Table of Contents: Abstract The Black Sea remains one of the largest underexplored rift basins in the world. Future success is dependent on a better understanding of a number of geological uncertainties. These include reservoir and source rock presence and quality, and the timing of migration of hydrocarbons relative to trap formation. An appreciation of the geological history of the Black Sea basins and the surrounding orogens is therefore key. The timing of basin formation, uplift of the margins, and of facies distribution remain issues for robust debate. This Special Publication presents the results of 15 studies that relate to the tectono-stratigraphy and petroleum geology of the Black Sea. The methodologies of these studies encompass crustal structure, geodynamic evolution, stratigraphy and its regional correlation, petroleum systems, source to sink, hydrocarbon habitat and play concepts, and reviews of past exploration. They provide insight into the many ongoing controversies concerning Black Sea regional geology and provide a better understanding of the geological risks that must be considered for future hydrocarbon exploration.
    Type of Medium: Monograph available for loan
    Pages: vii, 484 Seiten , farbige Illustrationen
    ISBN: 978-1-78620-358-8
    Series Statement: Geological Society Special Publication 464
    URL: http://sp.lyellcollection.org/content/464/1
    URL: http://sp.lyellcollection.org/content/specpubgsl/464/1.toc.pdf
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    BOOK
    Link to Library Catalog
    get availability status
  • 2
    Unknown
    Petroleum Geology of the Black Sea (2018)
    London : The Geological Society
    Details
    Keywords: Black Sea ; sedimentation ; petroleum geology
    Description / Table of Contents: Petroleum geology of the Black Sea: introduction / M. D. Simmons, G. C. Tari and A. I. Okay / Geological Society, London, Special Publications, 464, 1-18, 4 May 2018, https://doi.org/10.1144/SP464.15 --- Crustal structure and tectono-stratigraphy --- Crustal structure of the Mid Black Sea High from wide-angle seismic data / D. J. Shillington, T. A. Minshull, R. A. Edwards and N. White / Geological Society, London, Special Publications, 464, 19-32, 4 October 2017, https://doi.org/10.1144/SP464.6 --- Geological evolution of the Central Pontides / Aral I. Okay, Demir Altiner, Gürsel Sunal, Mesut Aygül, Remziye Akdoğan, Sevinç Altiner and Mike Simmons / Geological Society, London, Special Publications, 464, 33-67, 15 September 2017, https://doi.org/10.1144/SP464.3 --- Cretaceous geological evolution of the Pontides / Okan Tüysüz / Geological Society, London, Special Publications, 464, 69-94, 8 September 2017, https://doi.org/10.1144/SP464.9 --- Stratigraphy, petrogenesis and geodynamic setting of Late Cretaceous volcanism on the SW margin of the Black Sea, Turkey / Mehmet Keskİn and Okan Tüysüz / Geological Society, London, Special Publications, 464, 95-130, 28 September 2017, https://doi.org/10.1144/SP464.5 --- Geochronology, geochemistry and isotope systematics of a mafic–intermediate dyke complex in the İstanbul Zone. New constraints on the evolution of the Black Sea in NW Turkey / Namık Aysal, Mehmet Keskin, Irena Peytcheva and Olgun Duru / Geological Society, London, Special Publications, 464, 131-168, 25 September 2017, https://doi.org/10.1144/SP464.4 --- Hydrocarbon plays of the western Black Sea --- The geological history of the Istria ‘Depression’, Romanian Black Sea shelf: tectonic controls on second-/third-order sequence architecture / David R. D. Boote / Geological Society, London, Special Publications, 464, 169-209, 9 October 2017, https://doi.org/10.1144/SP464.8 --- Cretaceous sedimentation along the Romanian margin of the Black Sea: inferences from onshore to offshore correlations / C. Krezsek, R.-I. Bercea, G. Tari and G. Ionescu / Geological Society, London, Special Publications, 464, 211-245, 7 September 2017, https://doi.org/10.1144/SP464.10 --- Deep-water plays in the western Black Sea: insights into sediment supply within the Maykop depositional system / E. V. L. Rees, M. D. Simmons and J. W. P. Wilson / Geological Society, London, Special Publications, 464, 247-265, 15 September 2017, https://doi.org/10.1144/SP464.13 --- Regional petroleum systems and source rocks --- Oligocene and Lower Miocene source rocks in the Paratethys: palaeogeographical and stratigraphic controls / R. F. Sachsenhofer, S. V. Popov, A. Bechtel, S. Coric, J. Francu, R. Gratzer, P. Grunert, M. Kotarba, J. Mayer, M. Pupp, B. J. Rupprecht and S. J. Vincent / Geological Society, London, Special Publications, 464, 267-306, 7 September 2017, https://doi.org/10.1144/SP464.1 --- Source potential and depositional environment of Oligocene and Miocene rocks offshore Bulgaria / J. Mayer, B. J. Rupprecht, R. F. Sachsenhofer, G. Tari, A. Bechtel, S. Coric, W. Siedl, W. Kosi and J. Floodpage / Geological Society, London, Special Publications, 464, 307-328, 25 September 2017, https://doi.org/10.1144/SP464.2 --- Source rock evaluation of Middle Eocene–Early Miocene mudstones from the NE margin of the Black Sea / Stephen J. Vincent and Matthew N. D. Kaye / Geological Society, London, Special Publications, 464, 329-363, 25 September 2017, https://doi.org/10.1144/SP464.7 --- Messinian–Holocene stratigraphy --- Messinian canyons in the Turkish western Black Sea / N. Ö. Sipahioğlu and Z. Batı / Geological Society, London, Special Publications, 464, 365-387, 25 September 2017, https://doi.org/10.1144/SP464.12 --- Holocene source rock deposition in the Black Sea, insights from a dropcore study offshore Bulgaria / M. Fallah, J. Mayer, G. Tari and J. Baur / Geological Society, London, Special Publications, 464, 389-401, 15 September 2017, https://doi.org/10.1144/SP464.11 --- Petroleum potential of the eastern Black Sea and deep-water exploration review --- Stratigraphy, structure and petroleum exploration play types of the Rioni Basin, Georgia / G. Tari, D. Vakhania, G. Tatishvili, V. Mikeladze, K. Gogritchiani, S. Vacharadze, J. Mayer, C. Sheya, W. Siedl, J. J. M. Banon and J. L. Trigo Sanchez / Geological Society, London, Special Publications, 464, 403-438, 4 May 2018, https://doi.org/10.1144/SP464.14 --- History of deepwater exploration in the Black Sea and an overview of deepwater petroleum play types / G. C. Tari and M. D. Simmons / Geological Society, London, Special Publications, 464, 439-475, 4 May 2018, https://doi.org/10.1144/SP464.16
    Pages: Online-Ressource (VII, 484 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786203724
    URL: https://sp.lyellcollection.org/content/464/1
    Language: English
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    E-BOOK
  • 3
    Electronic Resource
    Electronic Resource
    Tectonic setting, petrology and geochronology of jadeite + glaucophane and chloritoid + glaucophane schists from north-west Turkey (1994)
    Oxford, UK : Blackwell Publishing Ltd
    Journal of metamorphic geology 12 (1994), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The north-west Turkish blueschists represent a subducted passive continental margin sequence dominated by metaclastic rocks and marble. The depositional age of the blueschist protoliths are probably Palaeozoic to Mesozoic, while the age of the high-pressure/low-temperature metamorphism is Late Cretaceous. Blueschists are tectonically overlain by a volcanosedimentary sequence made up of accreted oceanic crustal material that locally shows incipient blueschist metamorphism and by spinel peridotite slices.The metaclastic rocks with regional jadeite and glaucophane, which comprise the lower part of the blueschist unit, make up an over 1000-m-thick coherent sequence in the Kocasu region of north-west Turkey. Rare metabasic horizons in the upper parts of the metaclastic sequence with sodic amphibole + Iawsonite but no garnet indicate lawsonite blueschist facies metamorphism. The blueschist metaclastics in the Kocasu region are practically free of calcium and ferric iron and closely approximate the NFMASH system in bulk composition. Two low-variance mineral assemblages (with quartz and phengite) are jadeite + glaucophane + chlorite + paragonite and chloritoid + glaucophane + paragonite. The metaclastics comprise up to several-metres-thick layers of jadeite schist with quartz, phengite and nearly 100 mol% jadeite. Phase relations in the metaclastics show that the chloritoid + glaucophane assemblage, even in Fe2+-rich compositions, is stable in the jadeite stability field. In the NFASH system the above assemblage without the accompanying garnet has a narrow thermal stability field.Mineral equilibria in the metaclastics involving chloritoid, glaucophane, jadeite, paragonite and chlorite indicate metamorphic P-T conditions of 20 ± 2 kbar and 430 ± 30 d̀ C, yielding geothermal gradients close to 5d̀ C km-1, one of the lowest geotherms recorded. Blueschists in the Kocasu region, which have been buried to 70 km depth, are tectonically overlain by the volcanosedimentary sequence and by peridotite buried not deeper than 30 km.Phengites from two jadeite schists were dated by Ar/Ar laser probe; they give an age of 88.5 ± 0.5 Ma, interpreted as the age of metamorphism. Blueschists and the overlying peridotite bodies are intruded by 48-53-Ma-old granodiorite bodies that were emplaced at 10 km depth. This suggests that the exhumation of blueschists by underplating of cold continental crust, and normal faulting at the blueschist-peridotite, interface occurred during the Late Cretaceous to Palaeocene (88-53 Ma).
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1525-1314.1994.tb00035.x
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 4
    Electronic Resource
    Electronic Resource
    The oxygen fugacity stability of deerite: an alternative view (1987)
    Oxford, UK : Blackwell Publishing Ltd
    Journal of metamorphic geology 5 (1987), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1525-1314.1987.tb00401.x
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 5
    Electronic Resource
    Electronic Resource
    Paragonite eclogites from Dabie Shan, China: re-equilibration during exhumation? (1995)
    Oxford, UK : Blackwell Publishing Ltd
    Journal of metamorphic geology 13 (1995), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Paragonite in textural equilibrium with garnet, omphacite and kyanite is found in two eclogites in the ultrahigh-pressure metamorphic terrane in Dabie Shan, China. Equilibrium reactions between paragonite, omphacite and kyanite indicate a pressure of about 19 kbar at c. 700° C. However, one of the paragonite eclogites also contains clear quartz pseudomorphs after coesite as inclusions in garnet, suggesting minimum pressures of 27 kbar at the same temperature. The disparate pressure estimates from the same rock suggest that the matrix minerals in the ultrahigh-pressure eclogites have recrystallized at lower pressures and do not represent the peak ultrahigh-pressure assemblages. This hypothesis is tested by calibrating a garnet + zoisite/clinozoisite + kyanite + quartz/coesite geobarometer and applying it to the appropriate eclogite facies rocks from ultrahigh- and high-pressure terranes. These four minerals coexist from 10 to 60 kbar and in this wide pressure range the grossular content of garnet reflects the equilibrium pressure on the basis of the reaction zoisite/clinozoisite = grossular + kyanite + quartz/coesite + H2O. The results of the geobarometer agree well with independent pressure estimates from eclogites from other orogenic belts. For the paragonite eclogites in Dabie Shan the geobarometer indicates pressures in the quartz stability field, confirming that the former coesite-bearing paragonite-eclogite has re-equilibrated at lower pressures. On the other hand, garnets from other coesite-bearing but paragonite-free kyanite-zoisite eclogites show a very wide variation in grossular content, corresponding to a pressure variation from coesite into the quartz field. This wide variation, partly due to a rimward decrease in grossular component in garnet, is caused by partial equilibration of the mineral assemblage during the exhumation.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1525-1314.1995.tb00233.x
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 6
    Electronic Resource
    Electronic Resource
    Jadeite–chloritoid–glaucophane–lawsonite blueschists in north-west Turkey: unusually high P/T ratios in continental crust (2002)
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 20 (2002), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Sodic metapelites with jadeite, chloritoid, glaucophane and lawsonite form a coherent regional metamorphic sequence, several tens of square kilometres in size, and over a kilometre thick, in the Orhaneli region of northwest Turkey. The low-variance mineral assemblage in the sodic metapelites is quartz + phengite + jadeite + glaucophane + chloritoid + lawsonite. The associated metabasites are characterized by sodic amphibole + lawsonite ± garnet paragenesis. The stable coexistence of jadeite + chloritoid + glaucophane + lawsonite, not reported before, indicates metamorphic pressures of 24 ± 3 kbar and temperatures of 430 ± 30  °C for the peak blueschist facies conditions. These P–T conditions correspond to a geotherm of 5  °C km−1, one of the lowest recorded in continental crustal rocks. The low geotherm, and the known rate of convergence during the Cretaceous subduction suggest low shear stresses at the top of the downgoing continental slab.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1525-1314.2002.00402.x
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 7
    Electronic Resource
    Electronic Resource
    Alpine-Himalayan Blueschists (1989)
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 17 (1989), S. 55-87 
    Details
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1146/annurev.ea.17.050189.000415
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 8
    Electronic Resource
    Electronic Resource
    A fore-arc origin for the Thrace Basin, NW Turkey (1996)
    Springer
    International journal of earth sciences 85 (1996), S. 662-668 
    Details
    ISSN: 1437-3262
    Keywords: Fore-arc ; Medial Eocene ; Strike-slip Thrace ; Basin ; Turkey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Hydrocarbon-bearing Thrace Basin occupies much of the European part of Turkey. The Middle Eocene to Oligocene sequence in the centre of the basin exceeds 9 km in thickness. Based on the stratigraphy, structure and the regional context of this basin, we propose that it developed as a fore-arc basin between the medial Eocene and the Oligocene, above the northward subducting Intra-Pontide Ocean. Its post-Miocene history has been dominated mainly by wrench tectonics resulting from the activity of the now-deactivated northwestern strand. of the present-day North Anatolian fault zone.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02440103
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 9
    Electronic Resource
    Electronic Resource
    A fore-arc origin for the Thrace Basin, NW Turkey (1996)
    Springer
    Geologische Rundschau 85 (1996), S. 662-668 
    Details
    ISSN: 0016-7835
    Keywords: Key words Fore-arc ; Medial Eocene ; Strike-slip ; Thrace Basin ; Turkey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Hydrocarbon-bearing Thrace Basin occupies much of the European part of Turkey. The Middle Eocene to Oligocene sequence in the centre of the basin exceeds 9 km in thickness. Based on the stratigraphy, structure and the regional context of this basin, we propose that it developed as a fore-arc basin between the medial Eocene and the Oligocene, above the northward subducting Intra-Pontide Ocean. Its post-Miocene history has been dominated mainly by wrench tectonics resulting from the activity of the now-deactivated northwestern strand of the present-day North Anatolian fault zone.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s005310050104
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 10
    Electronic Resource
    Electronic Resource
    Sodic pyroxenes from metabasites in the eastern mediterranean (1978)
    Springer
    Contributions to mineralogy and petrology 68 (1978), S. 7-11 
    Details
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The compositions of sodic pyroxenes from blueschist metabasites in Northwest Turkey were investigated by electronprobe microanalysis. These are compared with sodic pyroxenes from high-grade blueschist terrains and eclogites with special reference to the island of Syros in Greece. Pyroxenes from lawsonite zone metabasites in Northwest Turkey are chloromelanites, aegerine augites and aegerine jadeites with the acmite contents ranging from 65% down to 30%. Epidote-garnet bearing high-grade blueschist metabasites of Syros on the other hand contain omphacite with the acmite content less than 30%. All the analyzed sodic pyroxenes from eclogites and high-grade blueschists in the literature are also omphacites with low acmite contents. It is argued that the acmite content of the sodic pyroxene decreases with rising temperature of metamorphism. This is almost entirely related to the appearance of epidote as an additional ferric ion bearing phase with an increase in temperature.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00375442
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...