Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

The record of seismic, hydroacoustic, and infrasonic waves is essential to detect, identify,
and localize sources of both natural and anthropogenic origin. To guarantee traceability and …

Earthquake swarms may be driven by fluids, through hydraulic injections or natural fluid
circulation, but also by slow and aseismic slip transients. Understanding the driving factors …

Anthropogenic fluid injections at depth induce seismicity which is generally organized as
swarms, clustered in time and space, with moderate magnitudes. Earthquake swarms also …

Abstract On 21 May 2021, an MS 6.4 earthquake occurred in Yangbi, Yunnan province,
China. A significant foreshock sequence occurred 3 days before the mainshock, which …

Abstract Since November 30, 2020, an intense seismic swarm and transient deformation
have been continuously observed in the Noto Peninsula, central Japan, which is a non …

Abstract The 2021 Mw 6.1 Yangbi earthquake in southwest China is preceded by three
major foreshocks: 05/18 Mw 4.3, 05/19 Mw 4.6, and 05/21 Mw 5.2. It provides a valuable …

Abstract The **aojiang Fault (XJF) Zone locates in the southeastern of Tibetan Plateau and
defines the boundary between the South China and Sichuan-Yunnan blocks. Historical …

Following laboratory experiments and friction theory, slow slip events and seismicity rate
accelerations observed before mainshocks are sometimes interpreted as evidence of a …

Identification of repeating earthquakes (repeaters) usually depends on waveform similarity
expressed as the corresponding cross‐correlation coefficient (CC) above a prescribed …