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  • 1
    Monograph available for loan
    Monograph available for loan
    Geological Evolution of Central Asian Basins and the Western Tien Shan Range (2017)
    London : Geological Society
    Associated volumes
    Details Availability
    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
    URL: http://sp.lyellcollection.org/content/427/1
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
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    Geological Evolution of Central Asian Basins and the Western Tien Shan Range (2017)
    London : The Geological Society
    Details
    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
    URL: http://sp.lyellcollection.org/content/427/1
    Language: English
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  • 3
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    Constraining Andean Propagation of Exhumation at the Limit of the Eastern Cordillera, NW Argentina, Using Low‐Temperature Thermochronology in a Structural Context (2022)
    Details
    Publication Date: 2022-12-07
    Description: Within the Central Andes of NW Argentina, the spatiotemporal distribution and style of deformation is strongly influenced by pre‐Cenozoic heterogeneities, mostly related to the Salta rift extension in the Cretaceous. At the enigmatic junction of the thin‐skinned Subandean belt and the thick‐skinned Santa Barbara System, the Tilcara Range and adjacent San Lucas block, located within the Eastern Cordillera, show thermochronological and field evidence of multiple exhumation events. Mesozoic (140‐115 Ma), pre‐Andean exhumation of basement highs is constrained by unconformities between basement and syn‐rift strata, as well as zircon (U‐Th‐Sm)/He cooling ages. Cenozoic Andean exhumation is quantified by apatite (U‐Th‐Sm)/He and fission track cooling ages, which were reset between the Late Cretaceous and Miocene. These data show that the westernmost Tilcara Range began exhuming in the late Oligocene‐early Miocene (26‐16 Ma), after which exhumation propagated to the border of the Eastern Cordillera in the middle Miocene (22‐10 Ma). The onset of rapid exhumation in the San Lucas block, which is located east of the Tilcara Range, occurred in the late Miocene (10‐8 Ma) in its western part, and in the late Miocene‐early Pliocene (6‐4 Ma) in its eastern part. Internal deformation of the San Lucas block, disturbing zircon (U‐Th‐Sm)/He and apatite fission track age patterns, predates propagation of rapid exhumation. The here presented low‐temperature thermochronology data set thus quantifies the multi‐phase exhumation history of the Eastern Cordillera of NW Argentina and constrains the timing of Andean propagation of exhumation within the Eastern Cordillera and the adjacent structural transition zone.
    Description: Key Points: Zircon (U‐Th‐Sm)/He data suggests that pre‐Andean exhumation of Salta rift basement highs occurred in the Early Cretaceous (140‐115 Ma). Apatite (U‐Th‐Sm)/He and fission track data indicate a late Oligocene‐early Miocene (26‐16 Ma) onset of exhumation in the Tilcara Range. Andean exhumation overall propagated in‐sequence eastward, but thermal models indicate the possibility of local out‐of‐sequence movement.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5281/zenodo.6358993
    Keywords: ddc:551.8 ; low‐temperature thermochronology ; thermal modeling ; structural geology ; Central Andes ; Eastern Cordillera ; Cenozoic
    Language: English
    Type: doc-type:article
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  • 4
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    Calc-alkaline volcanic rocks and zircon ages of the late Tonian: early Cryogenian arc-related Big Naryn Complex in the Eastern Djetim-Too Range, Middle Tianshan block, Kyrgyzstan (2020)
    Terbishalieva, Baiansuluu ; Timmerman, Martin Jan ; Mikolaichuk, Alexander ; [et al.]
    Springer Berlin Heidelberg
    Details
    Publication Date: 2023-06-19
    Description: The Big Naryn Complex (BNC) in the East Djetim-Too Range of the Kyrgyz Middle Tianshan block is a tectonized, at least 2 km thick sequence of predominantly felsic to intermediate volcanic rocks intruded by porphyric rhyolite sills. It overlies a basement of metamorphic rocks and is overlain by late Neoproterozoic Djetim-Too Formation sediments; these also occur as tectonic intercalations in the BNC. The up to ca. 1100 m thick Lower Member is composed of predominantly rhyolites-to-dacites and minor basalts, while the at least 900 m thick pyroclastic Upper Member is dominated by rhyolitic-to-dacitic ignimbrites. Porphyric rhyolite sills are concentrated at the top of the Lower Member. A Lower Member rhyolite and a sill sample have LA-ICP-MS U–Pb zircon crystallization ages of 726.1 ± 2.2 Ma and 720.3 ± 6.5 Ma, respectively, showing that most of the magmatism occurred within a short time span in the late Tonian–early Cryogenian. Inherited zircons in the sill sample have Neoarchean (2.63, 2.64 Ga), Paleo- (2.33–1.81 Ga), Meso- (1.55 Ga), and Neoproterozoic (ca. 815 Ma) ages, and were derived from a heterogeneous Kuilyu Complex basement. A 1751 ± 7 Ma 40Ar/39Ar age for amphibole from metagabbro is the age of cooling subsequent to Paleoproterozoic metamorphism of the Kuilyu Complex. The large amount of pyroclastic rocks, and their major and trace element compositions, the presence of Neoarchean to Neoproterozoic inherited zircons and a depositional basement of metamorphic rocks point to formation of the BNC in a continental magmatic arc setting.
    Description: Akademie Věd České Republiky http://dx.doi.org/10.13039/501100004240
    Description: Universität Potsdam (1031)
    Keywords: ddc:552.2 ; Tianshan orogenic belt ; Big Naryn complex ; Tonian–Cryogenian ; Magmatic arc ; Calc-alkaline ; Kuilyu complex
    Language: English
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  • 5
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    Cenozoic Exhumation and Deformation of the Intermontane Pastos Chicos Basin in the Southern Central Andes: Implications for the Tectonic Evolution of the Andean Plateau (Puna) and the Eastern Cordillera Between 23° and 24°S, NW Argentina (2023)
    Details
    Publication Date: 2023-07-04
    Description: The Andean Plateau of north‐western Argentina (Puna) at a mean elevation of ca. 4.2 km constitutes the southern continuation of the Altiplano; it is a compressional basin‐and‐range province comprising fault‐bounded, high‐elevation mountain ranges and largely internally drained basins with often thick sedimentary and volcaniclastic fill. Growing sedimentological and structural evidence supports the notion that the north‐western Argentine Andes between 22° and 26°S developed from an initial extensive broken‐foreland system that extended across the present‐day eastern Andean flank during the early to middle Eocene. However, compelling evidence of the tectonic history of this region is still missing. Here, we present new apatite fission track and zircon (U–Th)/He thermochronological data and U–Pb zircon ages from intercalated volcanic ash deposits from the Pastos Chicos Basin (23.5°S, 66.5°W) to constrain basin formation and the timing of major crustal deformation in the northern Puna. Inverse thermal modeling of the thermochronological data provides further temporal constraints on the late Cenozoic cooling history of the crust in this region and, by inference, on the timing of upper‐crustal shortening, range uplift, and basin formation in the northern sector of the present‐day Puna Plateau. Specifically, we argue for plateau‐wide distributed deformation in the Eocene between 23° and 24°S, followed by spatially disparate and diachronous deformation (Oligocene to Pliocene).
    Description: Plain Language Summary: The Argentine Puna Plateau is a mountainous region in the Central Andes of South America. It is the result of the tectonic convergence between the oceanic Nazca Plate and the continental South American Plate. However, the detailed tectonic evolution of this region is yet unknown. We present new thermochronologic data from the Puna Plateau that allow inferences about crustal deformation and mountain range uplift. Combined with previous studies, our results suggest deformation distributed over the entire plateau during the Eocene. Thereafter, local deformation occurred spatially non‐systematic, possibly related to zones of weakness in the crust.
    Description: Key Points: Thermal modeling of apatite fission track and (U‐Th)/He zircon data from the Pastos Chicos Basin shows Oligo‐Miocene onset of exhumation. Regional compilation of spatio‐temporal deformation at 23°–24°S suggests out‐of‐sequence deformation related to basement heterogeneities. Mio‐Pliocene U–Pb zircon ages of volcanic ash deposits refine the chronostratigraphy of the Pastos Chicos Basin.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Brandenburg Ministry of Sciences, Research and Cultural Affairs, Germany
    Description: Blaustein Fund
    Description: Fulbright Foundation
    Description: France‐Stanford Center for Interdisciplinary Studies
    Description: https://doi.org/10.6084/m9.figshare.20209865.v1
    Keywords: ddc:551.8 ; Puna Plateau ; NW Argentina ; thermochronology ; U–Pb zircon geochronology ; mountain range uplift ; Tectonics
    Language: English
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  • 6
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    Neogene aridification and lake development in the Issyk‐Kul basin, Kyrgyzstan (2023)
    Details
    Publication Date: 2023-11-24
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Uplift of the Tian Shan range modified regional climate during Cenozoic aridification in Central Asia. This study presents facies analyses and Neogene oxygen and carbon isotopic records from magnetostratigraphically dated terrestrial sedimentary sections on the southern side of the intermontane Issyk‐Kul basin in the Kyrgyz Tian Shan and 〈sup〉26〈/sup〉Al/〈sup〉10〈/sup〉Be isochron burial ages from the southern and eastern sides of the basin. The δ〈sup〉18〈/sup〉O and δ〈sup〉13〈/sup〉C data show a positive ca. 2‰ shift in values between ca. 8 and 7 Ma and a change from a negative to a positive trend. This change is attributed to the upwind growth of the Kyrgyz, Kungey and Trans Ili (Zaili) ranges, which diverted the westerlies, thereby changing the Issyk‐Kul basin from a windward to a leeward position, enhancing aridification and establishing the modern‐day spring and summer precipitation regime within the basin. Two 4 to 5 Ma 〈sup〉26〈/sup〉Al/〈sup〉10〈/sup〉Be isochron burial ages constrain the onset of Sharpyl Dak deposition on the eastern side of the basin; southward paleocurrent directions there suggest the eastward growth of the Kungey range in the Pliocene. Increased subsidence on the southern side of the basin and local tectonically induced river system reorganization led to the commencement of lake formation at ca. 5 Ma, followed by a ca. 2 Ma local depositional hiatus. The transition from sandstones of the Chu sedimentary group to conglomerates of the Sharpyl Dak group, marking a change from fluvial‐alluvial deposits to a proximal alluvial fan, is dated at 2.6–2.8 Ma by 〈sup〉26〈/sup〉Al/〈sup〉10〈/sup〉Be isochron burial dating on the southern side of the basin, driven either by tectonics or Northern Hemisphere glaciation. This study concludes that the late Miocene–Pliocene northward growth of Tian Shan significantly altered environmental conditions within the range, preventing the moisture‐bearing westerlies from reaching the intermontane Issyk‐Kul basin and promoting lake formation and expansion.〈/p〉
    Description: 〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉The late Miocene–Pliocene northward growth of Tian Shan created an orographic barrier that diverted the moisture‐bearing westerlies and enhanced aridification in the Issyk‐Kul basin. Reorganization of the river systems and enhanced subsidence led to the formation of an internally drained lake in Pliocene. The transition from sandstone to conglomerate (Sharpyl Dak group) deposition, linked to a change in climate and/or tectonic activity, occurred diachronously within the basin.〈boxed-text position="anchor" content-type="graphic" id="bre12751-blkfxd-0001" xml:lang="en"〉〈graphic position="anchor" id="jats-graphic-1" xlink:href="urn:x-wiley:0950091X:bre12751:bre12751-toc-0001"〉 〈/graphic〉〈/boxed-text〉〈/p〉
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: University of Wollongong http://dx.doi.org/10.13039/501100001777
    Keywords: ddc:551 ; Cenozoic aridification ; Central Asia ; cosmogenic 26Al/10Be ; tectonic uplift ; westerlies ; δ18O and δ13C stable isotopes
    Language: English
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  • 7
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    Measurement on single-grains for (U-Th)/He analysis of Ukrainian Carpathians LT thermochronometry (2023)
    PANGAEA
    Details
    Publication Date: 2023-09-08
    Keywords: (U-Th)He (AHe); Aliquot number; CAR19-029; CAR19-045; CAR19-047; CAR19-056; CAR19-061; CAR19-062; CAR19-063; CAR19-066; CAR19-068; CAR19-069; CAR19-072; Comment; Date; Dur930; Elevation of event; Event label; FCT102020; fission-track thermochronometry; Geological sample; GEOS; Latitude of event; Length; Longitude of event; Method comment; Mineral name; Number of pictures; Prism length; Sample code/label; Sample comment; Termination of grains; Ukrainian Carpathians; Width
    Type: Dataset
    Format: text/tab-separated-values, 1026 data points
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  • 8
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    Low-thermochronology data in the Ukrainian Carpathians wedge (2023)
    PANGAEA
    Details
    Publication Date: 2023-09-08
    Description: We wanted to model the time-temperature path of each tectonic unit of the Ukrainian Carpathians wedge to constrain the burial and accretion phase and assess the thermal evolution of the belt. During a field campaign in Ukraine in 2019, fourteen samples, weighing 3-5 kg each, were collected from sandstones across three transects in the Ukrainian Carpathians. Sampling focused on areas that were not targeted in previous studies (Andreucci et al., 2015; Nakapelyukh et al., 2018), aiming to collect at least one sample per tectonic unit along each transect. We conducted analysis for three thermochronometers; apatite fission-track (AFT), (U-Th)/He on apatite and on zircon grains (AHe and ZHe). Eleven of our samples gave statistically exploitable results. Most of the AHe single-grain are reset, whereas ZHe single-grain are mostly partially reset to fully non-reset. Aft ages are characterized by significant age dispersion (25-65 %), and are partially reset. During this work the author's contribution was as followed: AdL acquired funding for the project; AdL and MR planned the field campaign and sampled; MR and MB performed AFT analyses; ERS, MR and JG performed the AHe and ZHe measurements; ERS, MB and PvdB analyzed the data.
    Keywords: (U-Th)He (AHe); fission-track thermochronometry; Ukrainian Carpathians
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 9
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    Sample information of Ukrainian Carpathians LT thermochronometry (2023)
    PANGAEA
    Details
    Publication Date: 2023-09-08
    Keywords: (U-Th)He (AHe); CAR19-045; CAR19-047; CAR19-056; CAR19-061; CAR19-062; CAR19-063; CAR19-066; CAR19-068; CAR19-069; CAR19-070; CAR19-072; Elevation of event; Event label; fission-track thermochronometry; Geological sample; GEOS; Latitude of event; Lithology/composition/facies; Longitude of event; Stratigraphy; Tetonic unit; Thermochronometer; Ukrainian Carpathians
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 10
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    Fission-track apatite compiled data of Ukrainian Carpathians LT thermochronometry (2023)
    PANGAEA
    Details
    Publication Date: 2023-09-08
    Keywords: (U-Th)He (AHe); Age, fission-track; Age, mineral; Age, standard deviation; calculated, 2 sigma; CAR19-045; CAR19-056; CAR19-061; CAR19-062; CAR19-063; CAR19-066; CAR19-068; CAR19-069; CAR19-070; CAR19-072; Chi-squared; Dispersion; Elevation of event; Event label; Fission-track, Dpar; Fission-track, Dpar, standard error; Fission-track length, mean; Fission-track length, mean, standard deviation; Fission-tracks, dosimeter, density; Fission-tracks, induced; Fission-tracks, induced, density; Fission-tracks, spontaneous; Fission-tracks, spontaneous, density; fission-track thermochronometry; Geological sample; GEOS; Grains; Latitude of event; Longitude of event; Number; Ukrainian Carpathians; Uranium
    Type: Dataset
    Format: text/tab-separated-values, 157 data points
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