Crustal–lithospheric structure and continental extrusion of Tibet

MP Searle, JR Elliott, RJ Phillips… - Journal of the …, 2011 - lyellcollection.org
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 …

Crustal deformation in the India‐Eurasia collision zone from 25 years of GPS measurements

G Zheng, H Wang, TJ Wright, Y Lou… - Journal of …, 2017 - Wiley Online Library
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) …

Transformation of displacement between strike-slip and crustal shortening in the northern margin of the Tibetan Plateau: Evidence from decadal GPS measurements …

W Zheng, P Zhang, W He, D Yuan, Y Shao, D Zheng… - Tectonophysics, 2013 - Elsevier
Studies of Late Quaternary geological slip-rates and the GPS decadal slip-rates along the
major strike-slip faults in the northern margin of the Tibetan Plateau show that slip-rates …

[HTML][HTML] High-precision relocation of the aftershock sequence of the January 8, 2022, MS6. 9 Menyuan earthquake

L Fan, B Li, S Liao, C Jiang, L Fang - Earthquake Science, 2022 - Elsevier
Abstract The 2022 Menyuan MS 6.9 earthquake, which occurred on January 8, is the most
destructive earthquake to occur near the Lenglongling (LLL) fault since the 2016 Menyuan …

[HTML][HTML] 2022年1月8日青海门源MS6.9地震地表破裂带特征与发震机制

袁道阳, 谢虹, 苏瑞欢, 李智敏, 文亚猛, 司国军… - 地球物理学报, 2023 - dzkx.org
2022 年1 月8 日01 时45 分, 在青海省海北州门源县(N37. 77, E101. 26) 发生了MS 6.9 地震,
震源深度约10km. 震后现场考察确认, 本次地震震中位于祁连—海原断裂带中段的冷龙岭断裂与 …

Coseismic rupture model and tectonic implications of the January 7 2022, Menyuan Mw 6.6 earthquake constraints from InSAR observations and field investigation

Y Li, W Jiang, Y Li, W Shen, Z He, B Li, Q Li, Q Jiao… - Remote Sensing, 2022 - mdpi.com
A Mw 6.6 earthquake struck Menyuan, Qinghai, China, on 7 January 2022. To determine the
rupture parameters of this event, the coseismic InSAR deformation fields were mapped and …

Shallow creep on the Haiyuan fault (Gansu, China) revealed by SAR interferometry

R Jolivet, C Lasserre, MP Doin… - Journal of …, 2012 - Wiley Online Library
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 …

A New Tectonic Model for the 1927 M8.0 Gulang Earthquake on the NE Tibetan Plateau

P Guo, Z Han, F Gao, C Zhu, H Gai - Tectonics, 2020 - Wiley Online Library
The rupture patterns of large earthquakes in transpressional systems can provide important
information for understanding oblique motion and strain partitioning between tectonic …

Measurement of interseismic strain across the Haiyuan fault (Gansu, China), by InSAR

O Cavalié, C Lasserre, MP Doin, G Peltzer… - Earth and Planetary …, 2008 - Elsevier
The Haiyuan fault is part of a major left-lateral fault system at the northeastern edge of the
Tibet-Qinghai plateau. Two M8 earthquakes (1920 and 1927) occurred along the fault …

Strain Partitioning on the Western Haiyuan Fault System Revealed by the Adjacent 2016 Mw5.9 and 2022 Mw6.7 Menyuan Earthquakes

H Luo, T Wang - Geophysical Research Letters, 2022 - Wiley Online Library
Abstract The 1,000 km‐long Haiyuan fault is the largest strike‐slip fault system in the
northeastern Tibetan Plateau, accommodating part of the plateau's eastward extrusion …