We present a three‐dimensional electrical resistivity model of the crust and upper mantle
beneath the easternmost Kunlun fault (EKLf), obtained by three‐dimensional inversion of …

Located in the northeastern Tibetan Plateau, the East Kunlun fault is a west–east left-lateral
strike-slip fault that branches out into a horsetail-shaped structure known as the Kunlun …

Based on broadband magnetotelluric data collected in western Yunnan, we obtain a three‐
dimensional crustal resistivity model, which reveals seismogenic structures of Yingjiang and …

The Nantinghe fault zone is the largest northeast-trending fault of the active fault system in
southwestern Yunnan. Its tectonic activity and seismic hazard have attracted much attention …

Abstract A 2D Magnetotelluric (MT) profile (Sudian-Zhongshan MT profile) located at
Yingjiang-Longling area, western Yunnan, has been interpreted in refined processing …

The Longmenshan forms the eastern margin of the Tibetan Plateau adjacent to the Sichuan
Basin. This range is anomalous because it formed despite low convergence and slip rates …

The Xiaojiang fault system (XJFS), located to the southeast of the Tibetan Plateau, has a
complicated tectonic history and is an ideal location to study the Tibetan Plateau in terms of …

Abstract The 2008 Iwate-Miyagi Nairiku earthquake (M 7.2) was a shallow inland
earthquake that occurred in the volcanic front of the northeastern Japan arc. To understand …

Songyuan is the most earthquake prone area in northeast China. Since 2006, earthquakes
have occurred in the area in the form of swarms, with a maximum magnitude of M L5. 8 …

Abstract The region of South China mainly consists of the Yangtze block in the northwest,
the Cathaysia block in the southeast and the Jiangnan orogen in between these two major …