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  • 1
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 07.0421(312)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: vii, 352 S.
    ISBN: 9781862392717
    Series Statement: Geological Society special publication 312
    Classification:
    Regional Geology
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: 9/M 07.0421(427)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 605 Seiten , Illustrationen, graphische Darstellungen, Tabellen, Karten
    ISBN: 9781862397385
    Series Statement: Geological Society of London special publications 427
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Description / Table of Contents: The Upper Triassic to Middle Jurassic succession of the Shemshak Group (up to 4000 m in thickness in the Alborz Mountains, Northern Iran) contains key information about the closure of the Palaeotethys Ocean, the rise and denudation of the Cimmeride Mountains, and the succeeding opening of the South Caspian Basin. Here at Emamzadeh–Hashem Pass (NW of Tehran, Iran), the Shemshak Group is embraced between Upper Palaeozoic–Middle Triassic (foreground) and Upper Jurassic carbonates (background).
    Pages: Online-Ressource (VII, 352 Seiten)
    ISBN: 9781862392717
    Language: English
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  • 4
    Keywords: Central Asia ; Tien Shan ; basin formation ; geological evolution ; sedimentary basin ; climatic change
    Description / Table of Contents: Geological evolution of Central Asian Basins and the western Tien Shan Range / Marie-Françoise Brunet, Edward R. Sobel and Tom McCann / Geological Society, London, Special Publications, 427, 1-17, 14 July 2017, https://doi.org/10.1144/SP427.17 --- Regional evolution and extensional sedimentary basins --- Mesozoic tectonic and topographic evolution of Central Asia and Tibet: a preliminary synthesis / Marc Jolivet / Geological Society, London, Special Publications, 427, 19-55, 21 September 2015, https://doi.org/10.1144/SP427.2 --- Structural setting and evolution of the Afghan orogenic segment – a review / Agemar Siehl / Geological Society, London, Special Publications, 427, 57-88, 3 August 2015, https://doi.org/10.1144/SP427.8 --- Late Palaeozoic and Mesozoic evolution of the Amu Darya Basin (Turkmenistan, Uzbekistan) / Marie-Françoise Brunet, Andrey V. Ershov, Maxim V. Korotaev, Vladislav N. Melikhov, Eric Barrier, Dmitriy O. Mordvintsev and Irina P. Sidorova / Geological Society, London, Special Publications, 427, 89-144, 14 July 2017, https://doi.org/10.1144/SP427.18 --- Structure and evolution of the Bukhara-Khiva region during the Mesozoic: the northern margin of the Amu-Darya Basin (southern Uzbekistan) / Dmitriy Mordvintsev, Eric Barrier, Marie-Françoise Brunet, Christian Blanpied and Irina Sidorova / Geological Society, London, Special Publications, 427, 145-174, 3 May 2017, https://doi.org/10.1144/SP427.16 --- Subsidence history and basin-fill evolution in the South Caspian Basin from geophysical mapping, flexural backstripping, forward lithospheric modelling and gravity modelling / N. A. Abdullayev, F. Kadirov and I. S. Guliyev / Geological Society, London, Special Publications, 427, 175-196, 27 August 2015, https://doi.org/10.1144/SP427.5 --- Modelling the collisional and sedimentary evolution of the western part of the Tien Shan --- Crustal-scale structure of South Tien Shan: implications for subduction polarity and Cenozoic reactivation / C. Loury, Y. Rolland, S. Guillot, A. V. Mikolaichuk, P. Lanari, O. Bruguier and D. Bosch / Geological Society, London, Special Publications, 427, 197-229, 22 July 2015, https://doi.org/10.1144/SP427.4 --- The stratigraphic, sedimentological and structural evolution of the southern margin of the Kazakhstan continent in the Tien Shan Range during the Devonian to Permian / Dmitriy V. Alexeiev, Harry E. Cook, Alexandra V. Djenchuraeva and Alexander V. Mikolaichuk / Geological Society, London, Special Publications, 427, 231-269, 15 July 2015, https://doi.org/10.1144/SP427.3 --- Lithospheric structure in Central Eurasia derived from elevation, geoid anomaly and thermal analysis / Alexandra M. M. Robert, Manel Fernàndez, Ivone Jiménez-Munt and Jaume Vergés / Geological Society, London, Special Publications, 427, 271-293, 7 September 2015, https://doi.org/10.1144/SP427.10 --- Fault reactivation and far field effects --- Talas–Fergana Fault Cenozoic timing of deformation and its relation to Pamir indentation / Alejandro Bande, Edward R. Sobel, Alexander Mikolaichuk and Verónica Torres Acosta / Geological Society, London, Special Publications, 427, 295-311, 17 July 2015, https://doi.org/10.1144/SP427.1 --- Cenozoic palaeoenvironmental and tectonic controls on the evolution of the northern Fergana Basin / Alejandro Bande, Shukhrat Radjabov, Edward R. Sobel and Tatyana Sim / Geological Society, London, Special Publications, 427, 313-335, 18 December 2015, https://doi.org/10.1144/SP427.12 --- Sedimentation, environment and climate --- Integrated stratigraphy of a continental Pliensbachian–Toarcian Boundary (Lower Jurassic) section at Taskomirsay, Leontiev Graben, southwest Kazakhstan / Johann Schnyder, Denise Pons, Johan Yans, Romain Tramoy and Saya Abdulanova / Geological Society, London, Special Publications, 427, 337-356, 14 November 2016, https://doi.org/10.1144/SP427.15 --- Lower–Middle Jurassic facies patterns in the NW Afghan–Tajik Basin of southern Uzbekistan and their geodynamic context / Franz T. Fürsich, Marie-Françoise Brunet, Jean-Luc Auxiètre and Hermann Munsch / Geological Society, London, Special Publications, 427, 357-409, 6 August 2015, https://doi.org/10.1144/SP427.9 --- The Jurassic of the Western Tien Shan: the Central Kyzylkum Region, Uzbekistan / Tom McCann / Geological Society, London, Special Publications, 427, 411-437, 31 March 2016, https://doi.org/10.1144/SP427.13 --- The Cretaceous of the South Kyzylkum and Nuratau Region, Western Tien Shan, Central Uzbekistan / Tom McCann / Geological Society, London, Special Publications, 427, 439-489, 29 April 2016, https://doi.org/10.1144/SP427.14 --- The Upper Jurassic–Lower Cretaceous alluvial-fan deposits of the Kalaza Formation (Central Asia): tectonic pulse or increased aridity? / Marc Jolivet, Sylvie Bourquin, Gloria Heilbronn, Cecile Robin, Laurie Barrier, Marie-Pierre Dabard, Yingying Jia, Elien De Pelsmaeker and Bihong Fu / Geological Society, London, Special Publications, 427, 491-521, 21 September 2015, https://doi.org/10.1144/SP427.6 --- Cenozoic evolution of the Pamir and Tien Shan mountains reflected in syntectonic deposits of the Tajik Basin / M. Klocke, T. Voigt, J. Kley, S. Pfeifer, T. Rocktäschel, S. Keil and R. Gaupp / Geological Society, London, Special Publications, 427, 523-564, 11 September 2015, https://doi.org/10.1144/SP427.7 --- Late Eocene palaeogeography of the proto-Paratethys Sea in Central Asia (NW China, southern Kyrgyzstan and SW Tajikistan) / Roderic Bosboom, Oleg Mandic, Guillaume Dupont-Nivet, Jean-Noël Proust, Cholponbek Ormukov and Jovid Aminov / Geological Society, London, Special Publications, 427, 565-588, 7 September 2015, https://doi.org/10.1144/SP427.11
    Pages: Online-Ressource (VII, 605 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862397385
    Language: English
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  • 5
    Publication Date: 2009-04-06
    Description: A combination of fieldwork, basin analysis and modelling techniques has been used to try and understand the role, as well as the timing, of the subsidence-uplift mechanisms that have affected the Azerbaijan region of the South Caspian Basin (SCB) from Mesozoic to Recent. Key outcrops have been studied in the eastern Greater Caucasus, and the region has been divided into several major tectonic zones that are diagnostic of different former sedimentary realms representing a complete traverse from a passive margin setting to slope and distal basin environments. Subsequent deformation has caused folds and thrusts that generally trend from NW-SE to WNW-ESE. Offshore data has been analysed to provide insights into the regional structural and stratigraphic evolution of the SCB to the east of Azerbaijan. Several structural trends and subsidence patterns have been identified within the study area. In addition, burial history modelling suggests that there are at least three main components of subsidence, including a relatively short-lived basin-wide event at 6 Ma that is characterized by a rapid increase in the rate of subsidence. Numerical modelling that includes structural, thermal, isostatic and surface processes has been applied to the SCB. Models that reconcile the observed amount of fault-controlled deformation with the magnitude of overall thinning of the crust generate a comparable amount of subsidence to that observed in the basin. In addition, model results support the tectonic scenario that SCB crust has a density that is compatible with an oceanic composition and is being under-thrust beneath the central Caspian region.
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  • 6
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    In:  Geological Society Special Publication 312: 1-6.
    Publication Date: 2009-04-06
    Description: The structurally and stratigraphically complex area of northern and central Iran holds the key to understanding the plate tectonic evolution of the South Caspian-Central Iran area. The closure of the Palaeotethys, the opening of the Neotethys, the rise and demise of the Cimmerian mountain chain, as well as the onset of Neotethys subduction and large-scale Neotethyan back-arc rifting all predated the formation of the more than 20 km-thick fill of the South Caspian Basin. This volume brings together work by specialists in different disciplines of the geosciences (tectonics, geophysics, sedimentology, stratigraphy, palaeontology, basin modelling and geodynamics) in order to elucidate the complex Late Palaeozoic-Cenozoic geodynamic history of the Iran area and the birth of the South Caspian Basin.
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  • 7
    Publication Date: 2010-09-14
    Description: The Greater Caucasus is Europe's highest mountain belt and results from the inversion of the Greater Caucasus back-arc-type basin due to the collision of Arabia and Eurasia. The orogenic processes that led to the present mountain chain started in the Early Cenozoic, accelerated during the Plio-Pleistocene, and are still active as shown from present GPS studies and earthquake distribution. The Greater Caucasus is a doubly verging fold-and-thrust belt, with a pro- and a retro wedge actively propagating into the foreland sedimentary basin of the Kura to the south and the Terek to the north, respectively. Based on tectonic geomorphology - active and abandoned thrust fronts - the mountain range can be subdivided into several zones with different uplift amounts and rates with very heterogeneous strain partitioning. The central part of the mountain range - defined by the Main Caucasus Thrust to the south and backthrusts to the north - forms a triangular-shape zone showing the highest uplift and fastest rates, and is due to thrusting over a steep tectonic ramp system at depth. The meridional orogenic in front of the Greater Caucasus in Azerbaijan lies at the foothills of the Lesser Caucasus, to the south of the Kura foreland basin.
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  • 8
    Publication Date: 2012-01-01
    Description: Organic petrography and geochemical analyses have been carried out on shales, carbonaceous shales and coals of the Shemshak Group (Upper Triassic–Middle Jurassic) from 15 localities along the Alborz Range of Northern Iran. Thermal maturity of organic matter (OM) has been investigated using vitrinite reflectance, Rock-Eval pyrolysis and elemental analysis of kerogen. Reflectance of autochthonous vitrinite varies from 0.6 to 2.2% indicating thermally early-mature to over-mature OM in the Shemshak Group, in agreement with other maturity parameters used. The shales of the Shemshak Group are characterized by poor to high residual organic carbon contents (0.13 to 5.84%) and the presence of hydrogen-depleted OM, predominantly as a consequence of oxidation of OM at the time of deposition and the hydrogen loss during petroleum generation. According to light-reflected microscopy results, vitrinite/vitrinite-like macerals are dominant in the kerogen concentrates from the shaly facies. The coals and carbonaceous shales of the Shemshak Group show a wide range in organic carbon concentration (3.5 to 88.6%) and composition (inertinite- and vitrinite-rich types), and thereby different petroleum potentials. Thermal modelling results suggest that low to moderate palaeo-heat flow, ranging from 47 to 79 mW m-2 (57 mW m-2 on average), affected the Central-Eastern Alborz basin during Tertiary time, the time of maximum burial of the Shemshak Group. The maximum temperature that induced OM maturation of the Shemshak Group seems to be related to its deep burial rather than to a very strong heat flow related to an uppermost Triassic–Liassic rifting. The interval of petroleum generation in the most deeply buried part of the Shemshak Group (i.e. Tazareh section) corresponds to Middle Jurassic–Early Cretaceous times. Exhumation of the Alborz Range during Late Neogene time, especially along the axis of the Central-Eastern Alborz, where maximum vitrinite reflectance values are recorded, probably destroyed possible petroleum accumulations. However, on the northern flank of the Central-Eastern Alborz, preservation of petroleum accumulations may be expected. The northern part of the basin therefore seems the best target for petroleum exploration.
    Print ISSN: 0016-7568
    Electronic ISSN: 1469-5081
    Topics: Geosciences
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  • 9
    Publication Date: 2003-02-01
    Print ISSN: 0037-0738
    Electronic ISSN: 1879-0968
    Topics: Geosciences
    Published by Elsevier
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  • 10
    Publication Date: 2003-02-01
    Print ISSN: 0037-0738
    Electronic ISSN: 1879-0968
    Topics: Geosciences
    Published by Elsevier
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