The thermo-tectonic history of the Song-Kul plateau, Kyrgyz Tien Shan: Constraints by apatite and titanite thermochronometry and zircon U/Pb dating

Grave, Johan De; Glorie, Stijn; Buslov, M.M.; Izmer, Andrei; Fournier-Carrie, Alena; Batalev, V. Yu.; Vanhaecke, Frank; Elburg, Marlina; haute, Peter Van den

doi:10.1016/j.gr.2011.03.011

Cited by 123 publications

(69 citation statements)

References 68 publications

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“…The late Cenozoic thrust faults of the SW Chinese Tian Shan are likely transferred from the dextral TFF since ~15 Ma. (Bullen et al, 2001;Dumitru et atl., 2001;Sobel et al, 2006aSobel et al, , 2006bZhang et al, 2009;Glorie et al, 2010Glorie et al, , 2011De Grave et al, 2011Chang et al, 2012: Macaulay et al, 2014 Fig. 6 Thermal history modelling and confined track length distribution of TK-09…”

Section: Conlusionsmentioning

confidence: 99%

Cenozoic tectono-geomorphological growth of the SW Chinese Tian Shan: Insight from AFT and detrital zircon U–Pb data

Jia

Jolivet

et al. 2015

Journal of Asian Earth Sciences

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Section: Conlusionsmentioning

confidence: 99%

Cenozoic tectono-geomorphological growth of the SW Chinese Tian Shan: Insight from AFT and detrital zircon U–Pb data

Jia

Jolivet

et al. 2015

Journal of Asian Earth Sciences

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“…Using this technique, the zircon crystallization ages (closure-T $800-1000°C) of the sampled intrusives were determined in order to constrain the timing of pluton emplacement (Cherniak and Watson, 2003). The U/Pb analyses were carried out at the LA-ICP-(SF)-MS facility of the Department of Analytical Chemistry at Ghent University, using identical analytical procedures as those described in Glorie et al (2011b) andDe Grave et al (2011). The internal structure of the zircon crystals was investigated and mapped by cathodoluminescence (CL) imaging, using a JEOL JSM-6400 SEM (Scanning Electron Microscope).…”

Section: Zircon La-ic-ms U/pb Datingmentioning

confidence: 99%

“…The resulting AFT ages are cooling ages that can be linked to movements in the upper crust corresponding to exhumation and denudation of the sampled intrusions (e.g. De Grave and Van den haute, 2002; Glorie et al, 2010;De Grave et al, 2011;Jolivet et al, 2011). In this study, we followed the analytical procedures described by De Grave et al (2011) and Glorie et al (2011a).…”

Section: Apatite Fission Track Thermochronologymentioning

confidence: 99%

Tectonic history of the Irtysh shear zone (NE Kazakhstan): New constraints from zircon U/Pb dating, apatite fission track dating and palaeostress analysis

Glorie

Grave

Delvaux

et al. 2012

Journal of Asian Earth Sciences

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“…the Kyrgyz Tien Shan (e.g. Bullen et al, 2001;De Grave et al, 2011a, 2012Glorie et al, 2010Glorie et al, , 2011bKonopelko et al, 2007;Macaulay et al, 2014), the Chinese Junggar (e.g. Hendrix et al, 1992;Shen et al, 2012;Zhou et al, 2008) and the southern Altai (e.g.…”

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confidence: 99%

Late-Paleozoic emplacement and Meso-Cenozoic reactivation of the southern Kazakhstan granitoid basement

et al. 2015

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International audienceThe Ili-Balkhash Basin in southeastern Kazakhstan is located at the junction of the actively deforming mountain ranges of western Junggar and the Tien Shan, and is therefore part of the southwestern Central Asian Orogenic Belt. The basement of the Ili-Balkhash area consists of an assemblage of mainly Precambrian microcontinental fragments, magmatic arcs and accretionary complexes. Eight magmatic basement samples (granitoids and tuffs) from the Ili-Balkhash area were dated with zircon U-Pb LA-ICP-MS and yield Carboniferous to late Permian (~ 350-260 Ma) crystallization ages. These ages are interpreted as reflecting the transition from subduction to (post-) collisional magmatism, related to the closure of the Junggar-Balkhash Ocean during the Carboniferous – early Permian and hence, to the final late Paleozoic accretion history of the ancestral Central Asian Orogenic Belt. Apatite fission track (AFT) dating of 14 basement samples (gneiss, granitoids and volcanic tuffs) mainly provides Cretaceous cooling ages. Thermal history modeling based on the AFT data reveals that several intracontinental tectonic reactivation episodes affected the studied basement during the late Mesozoic and Cenozoic. Late Mesozoic reactivation and associated basement exhumation is interpreted as distant effects of the Cimmerian collisions at the southern Eurasian margin and possibly of the Mongol-Okhotsk Orogeny in SE Siberia during the Jurassic – Cretaceous. Following tectonic stability during the Palaeogene, inherited basement structures were reactivated during the Neogene (constrained by Miocene AFT ages of ~ 17–10 Ma). This late Cenozoic reactivation is interpreted as the far-field response of the India-Eurasia collision and reflects the onset of modern mountain building and denudation in southeast Kazakhstan, which seems to be at least partially controlled by the inherited basement architecture

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The thermo-tectonic history of the Song-Kul plateau, Kyrgyz Tien Shan: Constraints by apatite and titanite thermochronometry and zircon U/Pb dating

Cited by 123 publications

References 68 publications

Cenozoic tectono-geomorphological growth of the SW Chinese Tian Shan: Insight from AFT and detrital zircon U–Pb data

Cenozoic tectono-geomorphological growth of the SW Chinese Tian Shan: Insight from AFT and detrital zircon U–Pb data

Tectonic history of the Irtysh shear zone (NE Kazakhstan): New constraints from zircon U/Pb dating, apatite fission track dating and palaeostress analysis

Late-Paleozoic emplacement and Meso-Cenozoic reactivation of the southern Kazakhstan granitoid basement

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