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  • 1
    Call number: 9/M 07.0421(340)
    In: Geological Society special publication
    Description / Table of Contents: This wide area of the Alpine-Himalayan belt evolved through a series of tectonic events related to the opening and closure of the Tethys Ocean. In doing so it produced the largest mountain belt of the world, which extends from the Atlantic to the Pacific oceans. The basins associated with this belt contain invaluable information related to mountain building processes and are the locus of rich hydrocarbon accumulations. However, knowledge about the geological evolution of the region is limited compared to what they offer. This has been mainly due to the difficulty and inaccessibility of cross-country studies. This Special Publication is dedicated to the part of the Alpine Himalayan belt running from Bulgaria to Armenia, and from Ukraine to the Arabian Platform. It includes twenty multidisciplinary studies covering topics in structural geology/tectonics; geophysics; geochemistry; palaeontology; petrography; sedimentology; stratigraphy; and subsidence and lithospheric modelling. This volume reports results obtained during the MEBE (Middle East Basin Evolution) Programme and related projects in the circum Black Sea and peri-Arabian regions.
    Type of Medium: Monograph available for loan
    Pages: 509 S.
    ISBN: 9781862393080
    Series Statement: Geological Society special publication 340
    Classification:
    Sedimentology
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: 9/M 07.0421(428)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 368 Seiten
    ISBN: 9781862397392
    Series Statement: Geologial Society of London Special Publications 428
    Classification:
    Tectonics
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Description / Table of Contents: This wide area of the Alpine–Himalayan belt evolved through a series of tectonic events related to the opening and closure of the Tethys Ocean. In doing so it produced the largest mountain belt of the world, which extends from the Atlantic to the Pacific oceans. The basins associated with this belt contain invaluable information related to mountain building processes and are the locus of rich hydrocarbon accumulations. However, knowledge about the geological evolution of the region is limited compared to what they offer. This has been mainly due to the difficulty and inaccessibility of cross-country studies. This Special Publication is dedicated to the part of the Alpine–Himalayan belt running from Bulgaria to Armenia, and from Ukraine to the Arabian Platform. It includes twenty multidisciplinary studies covering topics in structural geology/tectonics; geophysics; geochemistry; palaeontology; petrography; sedimentology; stratigraphy; and subsidence and lithospheric modelling. This volume reports results obtained during the MEBE (Middle East Basin Evolution) Programme and related projects in the circum Black Sea and peri-Arabian regions.
    Pages: Online-Ressource (VII, 509 Seiten)
    ISBN: 9781862393080
    Language: English
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  • 4
    Keywords: tectonics ; Black Sea ; Caucasus
    Description / Table of Contents: Tectonic Evolution of the Eastern Black Sea and Caucasus: an introduction / Marc Sosson, Randell Stephenson and Shota Adamia / Geological Society, London, Special Publications, 428, 1-9, 9 June 2017, https://doi.org/10.1144/SP428.16 --- The ‘Caucasus’ domain --- Tectonic setting of Georgia–Eastern Black Sea: a review / S. A. Adamia, T. G. Chkhotua, T. T. Gavtadze, Z. A. Lebanidze, N. D. Lursmanashvili, N. G. Sadradze, D. P. Zakaraia and G. S. Zakariadze / Geological Society, London, Special Publications, 428, 11-40, 4 November 2015, https://doi.org/10.1144/SP428.6 --- From seafloor spreading to obduction: Jurassic–Cretaceous evolution of the northern branch of the Neotethys in the Northeastern Anatolian and Lesser Caucasus regions / M. Hässig, Y. Rolland and M. Sosson / Geological Society, London, Special Publications, 428, 41-60, 23 December 2015, https://doi.org/10.1144/SP428.10 --- Radiolarian evidence for the age of chert blocks from the Upper Cretaceous ophiolitic mélange unit of the Erakh area, Armenia / T. Danelian, G. Asatryan, L. Sahakyan, A. Avagyan and G. Galoyan / Geological Society, London, Special Publications, 428, 61-72, 14 December 2015, https://doi.org/10.1144/SP428.7 --- Geochemistry of the Eocene magmatic rocks from the Lesser Caucasus area (Armenia): evidence of a subduction geodynamic environment / L. Sahakyan, D. Bosch, M. Sosson, A. Avagyan, Gh. Galoyan, Y. Rolland, O. Bruguier, Zh. Stepanyan, B. Galland and S. Vardanyan / Geological Society, London, Special Publications, 428, 73-98, 3 February 2016, https://doi.org/10.1144/SP428.12 --- New data on the tectonic evolution of the Khoy region, NW Iran / Ara Avagyan, Alireza Shahidi, Marc Sosson, Lilit Sahakyan, Ghazar Galoyan, Carla Muller, Sargis Vardanyan, Khalil Bahar Firouzi, Delphine Bosch, Taniel Danelian, Gayane Asatryan, Mushegh Mkrtchyan and Mohammad Ali Shokri / Geological Society, London, Special Publications, 428, 99-116, 7 April 2016, https://doi.org/10.1144/SP428.13 --- Progressive orocline formation in the Eastern Pontides–Lesser Caucasus / Maud J. M. Meijers, Brigitte Smith, Daniel Pastor-Galán, Renzo Degenaar, Nino Sadradze, Shota Adamia, Lilit Sahakyan, Ara Avagyan, Marc Sosson, Yann Rolland, Cor G. Langereis and Carla Müller / Geological Society, London, Special Publications, 428, 117-143, 27 October 2015, https://doi.org/10.1144/SP428.8 --- Onset of Maikop sedimentation and cessation of Eocene arc volcanism in the Talysh Mountains, Azerbaijan / A. van der Boon, K. F. Kuiper, G. Villa, W. Renema, M. J. M. Meijers, C. G. Langereis, E. Aliyeva and W. Krijgsman / Geological Society, London, Special Publications, 428, 145-169, 29 October 2015, https://doi.org/10.1144/SP428.3 --- Growth structures, piggy-back basins and growth strata of the Georgian part of the Kura foreland fold–thrust belt: implications for Late Alpine kinematic evolution / V. M. Alania, A. O. Chabukiani, R. L. Chagelishvili, O. V. Enukidze, K. O. Gogrichiani, A. N. Razmadze and N. S. Tsereteli / Geological Society, London, Special Publications, 428, 171-185, 27 October 2015, https://doi.org/10.1144/SP428.5 --- Thermochronometric evidence for Miocene tectonic reactivation of the Sevan–Akera suture zone (Lesser Caucasus): a far-field tectonic effect of the Arabia–Eurasia collision? / W. Cavazza, I. Albino, M. Zattin, G. Galoyan, N. Imamverdiyev and R. Melkonyan / Geological Society, London, Special Publications, 428, 187-198, 27 October 2015, https://doi.org/10.1144/SP428.4 --- The ‘Black Sea’ domain --- DOBRE-2 WARR profile: the Earth's upper crust across Crimea between the Azov Massif and the northeastern Black Sea / V. Starostenko, T. Janik, R. Stephenson, D. Gryn, O. Rusakov, W. Czuba, P. Środa, M. Grad, A. Guterch, E. Flüh, H. Thybo, I. Artemieva, A. Tolkunov, G. Sydorenko, D. Lysynchuk, V. Omelchenko, K. Kolomiyets, O. Legostaeva, A. Dannowski and A. Shulgin / Geological Society, London, Special Publications, 428, 199-220, 3 February 2016, https://doi.org/10.1144/SP428.11 --- Local tomography model of the northeastern Black Sea: intra-plate crustal underthrusting / Valentina Gobarenko, Tamara Yegorova and Randell Stephenson / Geological Society, London, Special Publications, 428, 221-239, 27 October 2015, https://doi.org/10.1144/SP428.2 --- Mesozoic to recent geological history of southern Crimea and the Eastern Black Sea region / A. M. Nikishin, M. Wannier, A. S. Alekseev, O. A. Almendinger, P. A. Fokin, R. R. Gabdullin, A. K. Khudoley, L. F. Kopaevich, A. V. Mityukov, E. I. Petrov and E. V. Rubtsova / Geological Society, London, Special Publications, 428, 241-264, 27 October 2015, https://doi.org/10.1144/SP428.1 --- Key problems of stratigraphy in the Eastern Crimea Peninsula: some insights from new dating and structural data / Yevgeniya Sheremet, Marc Sosson, Carla Muller, Oleg Gintov, Anna Murovskaya and Tamara Yegorova / Geological Society, London, Special Publications, 428, 265-306, 7 April 2016, https://doi.org/10.1144/SP428.14 --- Geological structure of the northern part of the Eastern Black Sea from regional seismic reflection data including the DOBRE-2 CDP profile / G. Sydorenko, R. Stephenson, T. Yegorova, V. Starostenko, A. Tolkunov, T. Janik, M. Majdanski, Z. Voitsitskiy, O. Rusakov and V. Omelchenko / Geological Society, London, Special Publications, 428, 307-321, 23 May 2016, https://doi.org/10.1144/SP428.15 --- Stratigraphic comparisons along the Pontides (Turkey) based on new nannoplankton age determinations in the Eastern Pontides: geodynamic implications / J.-C. Hippolyte, C. Müller, E. Sangu and N. Kaymakci / Geological Society, London, Special Publications, 428, 323-358, 27 October 2015, https://doi.org/10.1144/SP428.9
    Pages: Online-Ressource (VI, 368 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862397392
    Language: English
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  • 5
    ISSN: 1573-0581
    Keywords: Oblique subduction ; strike-slip faults ; transpressive deformation ; tectonic erosion ; tectonic accretion ; seamount collision ; multibeam bathymetry
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The southern Kermadec-Hikurangi convergent margin, east of New Zealand, accommodates the oblique subduction of the oceanic Hikurangi Plateau at rates of 4–5 cm/yr. Swath bathymetry and sidescan data, together with seismic reflection and geopotential data obtained during the GEODYNZ-SUD cruise, showed major changes in tectonic style along the margin. The changes reflect the size and abundance of seamounts on the subducting plateau, the presence and thickness of trench-fill turbidites, and the change to increasing obliquity and intracontinental transpression towards the south. In this paper, we provide evidence that faulting with a significant strike-slip component is widespread along the entire 1000 km margin. Subduction of the northeastern scrap of the Hikurangi Plateau is marked by an offset in the Kermadec Trench and adjacent margin, and by a major NW-trending tear fault in the scarp. To the south, the southern Kermadec Trench is devoid of turbidite fill and the adjacent margin is characterized by an up to 1200 m high scarp that locally separates apparent clockwise rotated blocks on the upper slope from strike-slip faults and mass wasting on the lower slope. The northern Hikurangi Trough has at least 1 km of trench-fill but its adjacent margin is characterized by tectonic erosion. The toe of the margin is indented by 10–25 km for more than 200 km, and this is inferred to be the result of repeated impacts of the large seamounts that are abundant on the northern Hikurangi Plateau. The two most recent impacts have left major indentations in the margin. The central Hikurangi margin is characterized by development of a wide accretionary wedge on the lower slope, and by transpression of presubduction passive margin sediments on the upper slope. Shortening across the wedge together with a component of strike-slip motion on the upper slope supports an interpretation of some strain partitioning. The southern Hikurangi margin is a narrow, mainly compressive belt along a very oblique, apparently locked subduction zone.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1573-0581
    Keywords: New Zealand ; Puysegur Trench ; Puysegur Ridge ; swath bathymetry ; oblique subduction ; strike-slip
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The Geodynz-sud cruise on board the R/V l'Atalante collected bathymetric, side-scan sonar and seismic reflection data along the obliquely convergent boundary between the Australian and Pacific plates southwest of the South Island, New Zealand. The survey area extended from 44°05′ S to 49°40′ S, covering the transition zone between the offshore extension of the Alpine Fault and the Puysegur Trench and Puysegur Ridge. Based on variations in the nature and structure of the crust on either side of the margin, the plate boundary zone can be divided into three domains with distinctive structural and sedimentary characteristics. The northern domain involves subduction of probably thinned continental crust of the southern Challenger Plateau beneath the continental crust of Fiordland. It is characterized by thick sediments on the downgoing slab and a steep continental slope disrupted by fault scarps and canyons. The middle domain marks the transition between subduction of likely continental and oceanic crust defined by a series of en echelon ridges on the downgoing slab. This domain is characterized by a large collapse terrace on the continental slope which appears to be due to the collision of the en echelon ridges with the plate margin. The southern domain involves subduction of oceanic crust beneath continental and oceanic crust. This domain is characterized by exposed fabric of seafloor spreading on the downgoing slab, a steep inner trench wall and linear ridges and valleys on the Puysegur ridge crest. The data collected on this cruise provide insights into the nature and history of both plates, and factors influencing the distribution of strike-slip and compressive strain and the evolution of subduction processes along a highly oblique convergent margin.
    Type of Medium: Electronic Resource
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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: 2010-09-14
    Description: The stress indicators describing the recent (provided by active tectonics framework) and palaeo-stress (provided by micro-fault kinematics and volcanic cluster) patterns show the scale and temporal changes in stress states since the beginning of Arabian-Eurasian collision. The recent stress derived from the active fault kinematics in the Lesser Caucasus and adjacent area corresponds to a strike-slip regime with both transtension and transpression characteristics. The kinematics of active structures of various scale are conditioned by tectonic stress field with general north-south compression and east-west extension. The distribution of Neogene to Quaternary volcanic cluster geometries and micro-fault kinematic data evidence the time and orientation variability of the stress field since the beginning of the Arabian-Eurasian collision. In addition to the general north-south compression orientation, two other - NW-SE and NE-SW - secondary orientations are observed. The first one was dominant between the Palaeogene and the late Early Miocene and the second one has prevailed between the Late Miocene and the Quaternary. Since the continental collision of Arabia with Eurasia the tectonic stress regime in the Lesser Caucasus and adjacent area changed from compression (thrusting and reverse faulting) to transtension-transpression (strike-slip faulting with various vertical components).
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  • 9
    Publication Date: 2010-09-14
    Description: The Palaeozoic to recent evolution of the Tethys system gave way to the largest mountain chain of the world extending from the Atlantic to Pacific oceans - the Alpine-Himalayan Mountain chain, which is still developing as a result of collision and northwards convergence of continental blocks including Apulia in the west, the Afro-Arabian Plate in the middle and the Indian Plate in the east. This Special Publication addresses the main problems of the middle part of this system incorporating the Balkans, Black Sea and Greater Caucasus in the north and the Afro-Arabian Plate in the south. Since the Early Mesozoic a number of small to large scale oceanic basins opened and closed as the intervening continental fragments drifted northwards and diachronously collided with and accreted to the southern margin of the Eurasian Plate. Despite the remarkable consequences of this, in terms of subduction, obduction and orogenic processes, little is known about the timing and palaeogeographic evolution of the region. This includes the amounts of shortening and interplay between synconvergent extension and compression, development of magmatic arc and arc-related basins and the timing and mechanism of their deformation. The chapters presented in this Special Publication present new information that help to fill some of the gaps of the puzzle.
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  • 10
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