Crustal–lithospheric structure and continental extrusion of Tibet
Crustal shortening and thickening to c. 70–85 km in the Tibetan Plateau occurred both
before and mainly after the c. 50 Ma India–Asia collision. Potassic–ultrapotassic shoshonitic …
before and mainly after the c. 50 Ma India–Asia collision. Potassic–ultrapotassic shoshonitic …
Crustal deformation in the India‐Eurasia collision zone from 25 years of GPS measurements
Abstract The India‐Eurasia collision zone is the largest deforming region on the planet;
direct measurements of present‐day deformation from Global Positioning System (GPS) …
direct measurements of present‐day deformation from Global Positioning System (GPS) …
Active faulting, mountain growth, and erosion at the margins of the Tibetan Plateau constrained by in situ-produced cosmogenic nuclides
R Hetzel - Tectonophysics, 2013 - Elsevier
The India–Asia collision zone is a key area for understanding continental plateau formation
and mountain building. Two fundamental questions in this context are how the …
and mountain building. Two fundamental questions in this context are how the …
Kinematic slip evolution during the 2022 Ms 6.8 Luding, China, earthquake: Compatible with the preseismic locked patch
R Guo, L Li, W Zhang, Y Zhang, X Tang… - Geophysical …, 2023 - Wiley Online Library
Abstract The September 2022 Ms 6.8 Luding earthquake broke more than 230 years of
seismic calm on the Moxi fault, providing a unique opportunity to understand its seismogenic …
seismic calm on the Moxi fault, providing a unique opportunity to understand its seismogenic …
Spatial slip rate distribution along the SE **anshuihe fault, eastern Tibet, and earthquake hazard assessment
The **anshuihe (XSH) fault in eastern Tibet is one of the most active faults in China, with the
next large earthquake most likely to occur along its SE part, where the fault splits into three …
next large earthquake most likely to occur along its SE part, where the fault splits into three …
Southeastward increase of the late Quaternary slip-rate of the **anshuihe fault, eastern Tibet. Geodynamic and seismic hazard implications
The left-lateral strike-slip **anshuihe fault system located in the eastern Tibetan Plateau is
considered as one of the most tectonically active intra-continental fault system in China …
considered as one of the most tectonically active intra-continental fault system in China …
Heterogeneous interseismic coupling along the **anshuihe‐**aojiang fault system, eastern Tibet
Abstract We use Global Positioning System (GPS) and Interferometric Synthetic Aperture
Radar (InSAR) data to quantify the interseismic coupling along the **anshuihe‐**aojiang …
Radar (InSAR) data to quantify the interseismic coupling along the **anshuihe‐**aojiang …
Shallow creep on the Haiyuan fault (Gansu, China) revealed by SAR interferometry
Interferometric synthetic aperture radar data are used to map the interseismic velocity field
along the Haiyuan fault system (HFS), at the north‐eastern boundary of the Tibetan plateau …
along the Haiyuan fault system (HFS), at the north‐eastern boundary of the Tibetan plateau …
Rupture kinematics and coseismic slip model of the 2021 Mw 7.3 Maduo (China) earthquake: Implications for the seismic hazard of the Kunlun fault
H Chen, C Qu, D Zhao, C Ma, X Shan - Remote Sensing, 2021 - mdpi.com
The 21 May 2021 Maduo earthquake was the largest event to occur on a secondary fault in
the interior of the active Bayanhar block on the north-central Tibetan plateau in the last …
the interior of the active Bayanhar block on the north-central Tibetan plateau in the last …
Geodetic imaging of shallow creep along the **anshuihe fault and its frictional properties
X Qiao, Y Zhou - Earth and Planetary Science Letters, 2021 - Elsevier
The **anshuihe fault is one of the most tectonically active faults in the eastern Tibetan
plateau. Understanding its slip behaviour and frictional properties is essential for …
plateau. Understanding its slip behaviour and frictional properties is essential for …