Ambient noise tomography is one of the most important breakthroughs in seismological
research since the 21st century. The method does not depend on the occurrence of natural …

From 2011 to 2013, the CHINArray project led by the Institute of Geophysics, China
Earthquake Administration, made the first phase deployment of 350 broadband …

P‐wave microseisms are excited by ocean swell activities. The recent development of an
ocean wave model allows us to compare them quantitatively. For the comparison, a single …

Southeast Tibet provides a weak window for continental extrusion and plateau expansion,
yet there is still limited understanding regarding specific deformation patterns in this region …

High-quality datasets are critical for the development of advanced machine-learning
algorithms in seismology. Here, we present an earthquake dataset based on the ChinArray …

Microseisms are the most energetic signals of Earth's ambient noise field. Locating the
sources of microseisms helps us to understand arrivals on noise cross‐correlation functions …

背景噪声成像技术是21 世纪以来地震学研究最为重要的突破性进展之一. 该方法不依赖于天然
地震事件的发生, 利用连续地震记录中普遍存在的“背景噪声”, 通过不同台站对间连续时间信号的 …

We conduct a systematic detection of microseismicity around Yunnan Province, Southwest
China following the 2004 Mw9. 1 Sumatra and 2012 Mw8. 6 Indian Ocean earthquakes …

Using continuous data from a dense seismic array in Southwestern China, we tracked S‐
wave microseism sources generated by two storms in Southeast Australia and the North …

Ambient noise technology can efficiently extract surface wave signals from seismic
background noise and has been extensively utilized in imaging lithospheric structures …