The deformation mode of the Tibetan Plateau is of crucial importance for understanding its
construction and extrusion processes, as well as for the assessment of regional earthquake …

The postseismic deformation mechanism is crucial for understanding the evolution of
postseismic crustal stress, strain, and aftershocks. Here, we used∼ 1 year Sentinel-1 data to …

We image the rupture process of the 2021 Mw 7.4 Maduo, Tibet earthquake using slowness‐
enhanced back‐projection (BP) and joint finite fault inversion, which combines teleseismic …

A finite-fault earthquake slip model can characterize the kinematics of rupture, which is
essential for earthquake mechanism studies and seismic hazard assessments. The finite …

Abstract On 22 May 2021, an earthquake (98.3 E and 34.59 N) struck Maduo town in
Qinghai province, occurring along a relatively obscure secondary fault within the block. We …

Abstract On September 5, 2022, a M6. 8 earthquake occurred in Luding county, Sichuan
Province. The epicenter is located at the southeastern end of the **anshuihe fault. The …

Abstract On 22 May 2021, at 2: 40 am (local time), an earthquake with a moment magnitude
of 7.4 was reported to have occurred in Maduo County (34.59° N, 98.34° E), China. The …

Coseismic slip and early post-earthquake afterslip are important ways to observe
seismogenic morphology and friction properties of seismogenic faults. We use InSAR data to …

Geodetic observations and seismic inversions suggest that the 2021 Mw7. 4 Maduo
earthquake's rupture velocity differs in two directions. However, the dynamic mechanisms …

To explore the degree of constraint by Global Navigation Satellite System (GNSS) and
Interferometric Synthetic Aperture Radar (InSAR) data on the Maduo earthquake within a …