Late Cenozoic thrust propagation within the Keping fold-and-thrust belt along the southern foreland of Chinese Tian Shan: Evidence from apatite (U Th)/He results

2021 ◽  
pp. 228966
Author(s):  
Lixing Lü ◽  
Jimin Sun ◽  
Yingying Jia ◽  
Lin Wu
Tectonics ◽  
2019 ◽  
Vol 38 (6) ◽  
pp. 2036-2058 ◽  
Author(s):  
Zhiliang Zhang ◽  
Jimin Sun ◽  
Lixing Lü ◽  
Shengchen Tian ◽  
Mengmeng Cao ◽  
...  

2019 ◽  
Vol 131 ◽  
pp. 101647
Author(s):  
Delong Ma ◽  
Hemin A. Koyi ◽  
Jianying Yuan ◽  
Dengfa He ◽  
Huquan Zhang ◽  
...  

Tectonics ◽  
2006 ◽  
Vol 25 (3) ◽  
pp. n/a-n/a ◽  
Author(s):  
Christine Authemayou ◽  
Dominique Chardon ◽  
Olivier Bellier ◽  
Zaman Malekzadeh ◽  
Esmaeil Shabanian ◽  
...  

2019 ◽  
Vol 766 ◽  
pp. 416-432 ◽  
Author(s):  
Jian Chang ◽  
Dan Li ◽  
Kyoungwon Min ◽  
Nansheng Qiu ◽  
Yao Xiao ◽  
...  

Author(s):  
Yuqing He ◽  
Teng Wang ◽  
Lihua Fang ◽  
Li Zhao

Abstract The Keping-tage fold-and-thrust belt in southwest Tian Shan is seismically active, yet the most well-recorded earthquakes occurred south of the mountain front. The lack of large earthquakes beneath the fold-and-thrust belt thus hinders our understanding of the orogenic process to the north. The 2020 Mw 6.0 Jiashi earthquake is an important event with surface deformation in the fold-and-thrust belt well illuminated by Interferometric Synthetic Aperture Radar, providing an opportunity to study the present-day kinematics of the thrust front through the analysis of satellite measurements of surface deformations. Here, we employ the surface deformation and relocated aftershocks to investigate the fault-slip distribution associated to this event. Further added by an analysis of Coulomb stress changes, we derive a fault model involving slips on a shallow, low-angle (∼10°) north-dipping thrust fault as well as on a left-lateral tear fault and a high-angle south-dipping reverse fault in mid-crust. Aftershocks at depth reflect the basement-involved shortening activated by a thin-skinned thrust faulting event. In addition, this earthquake uplifted the southernmost mountain front with relatively low topography, indicating the basin-ward propagation of the southwest Tian Shan.


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