Tectonic research of the Tibetan Plateau has long focused on its deformation style and
mechanisms. The 2008 Mw7. 9 Wenchuan earthquake ruptured the Longmen Shan fault …

Seismic and field observations indicate that the M w 7.4 Maduo earthquake ruptured the
Jiangcuo fault, which is a secondary fault∼ 85 km south of the northern boundary of the …

Several seismic gaps have been identified along the **anshuihe-**aojiang fault zone and
the Longmenshan fault zone in the Sichuan-Yunnan region, including the Daofu-Shimian …

We investigated the spatial distribution of aseismic creep on the Laohushan‐Haiyuan fault
using Global Positioning System (GPS) data (1999–2017) and Interferometric Synthetic …

We model the time‐dependent postseismic displacements following the 2001 Mw7. 8
Kokoxili earthquake, including both GPS (2001–2002 for near‐field and 2001–2010 for far …

Aseismic afterslip is postseismic fault sliding that may significantly redistribute crustal
stresses and drive aftershock sequences. Afterslip is typically modeled through geodetic …

Lithospheric geophysical exploration, structural imaging and anisotropy are the basis for the
study of continental dynamics of the Tibetan Plateau. In recent years, with the advancement …

The seismic hazard of a fault system is controlled by the maximum possible earthquake
magnitude it can host. However, existing methods to estimate maximum magnitudes can …

Qilian-Haiyuan fault zone, the boundary fault zone of the northeastern margin of the Tibetan
plateau, regulates the northeastward spreading of the Tibetan plateau and the eastward …

Abstract On May 22, 2021, a MW 7.4 event stroke Qinghai Madoi in Bayan Har massif,
attracting attention on the seismic activities in this area. Based on a campaign-mode …