The sedimentary basin is a basic geological unit in the Earth system: its formation and
evolution are controlled mainly by plate tectonics and geodynamics, which have produced a …

Earthquake interaction across multiple time scales can reveal complex stress evolution and
rupture patterns. Here, we investigate the role of static stress change in the 2023 Mw 7.8 and …

Abstract The Jiaodong Peninsula, located in the eastern North China Craton (NCC), is a key
region to study the genetic linkage between large-scale gold mineralization and craton …

North China is characterized by numerous faults, where many earthquakes were recorded.
However, the fault slip and crustal deformation mechanism underlying the effects of …

Abstract The Tan-Lu Fault Zone (TLFZ), East China, is the site of several historical M 6.5–8.0
earthquakes and remains seismically active today. Although differential kinematic and …

Deterministic ground motions up to 0.5 Hz from a set of spontaneous dynamic ruptures of M
w 7.5 scenario earthquakes on a 160‐km right‐lateral seismic gap in the north China basin …

The tectonic stress field in the middle-upper crust is closely related to the structure and
rheology of the lithosphere. To determine the stress field in the deep crust, we inversed the …

Abstract The Zhangjiakou-Bohai Seismic Belt (ZBSB) is a crucial intraplate seismic belt in
Eastern China, covering densely populated and economically developed regions with …

North China is characterized by significant lithosphere heterogeneity and numerous faults,
with the occurrence of many historical and ongoing devastating earthquakes. To extend our …

A 160 km long seismic gap, which has not been ruptured over~ 8000 years, was identified
recently in North China. In this study, we use a dynamic source model and a newly available …