9 Papers
20 Citations
C. Li is an academic researcher from Georgia Institute of Technology. The author has contributed to research in topics: Aftershock & Induced seismicity. The author has an hindex of 5, co-authored 8 publications.
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Papers
Deep learning for seismic phase detection and picking in the aftershock zone of 2008 Mw7.9 Wenchuan Earthquake
Lijun Zhu,Zhigang Peng,James H. McClellan,C. Li,D. Yao,D. Yao,Zefeng Li,Zefeng Li,Lihua Fang +8 more
TL;DR: In this paper, a CNN-based phase identification classifier (CPIC) was proposed for phase detection and picking on small to medium sized training datasets, and applied to one-month continuous recordings during the aftershock sequences of the 2008 M_W 7.9 Wenchuan Earthquake in Sichuan, China, CPIC detects 97.5% of the manually picked phases in the standard catalog and predicts their arrival times with a five times improvement over the ObsPy AR picker.
122
The 2018 Fiji Mw 8.2 and 7.9 deep earthquakes: One doublet in two slabs
TL;DR: In this paper, a doublet with moment magnitude (M w ) 8.2 and 7.9 occurred in a warm relic slab leaning on top of the Tonga slab.
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Detecting remotely triggered microseismicity around Changbaishan Volcano following nuclear explosions in North Korea and large distant earthquakes around the world
TL;DR: In this article, the authors conduct a systematic survey on locally triggered earthquakes by large distant earthquakes in Changbaishan Volcano, an active intraplate volcano on the border between China and North Korea.
21
Long‐Period Long‐Duration Events Detected by the IRIS Community Wavefield Demonstration Experiment in Oklahoma: Tremor or Train Signals?
TL;DR: In this article, a local similarity method was applied to detect long-period long-duration (LPLD) seismic events using 1-month continuous waveforms recorded by a nodal array from the Incorporated Research Institutions for Seismology (IRIS) community wavefield experiment in Oklahoma.
17
Abundant aftershock sequence of the 2015 Mw7.5 Hindu Kush intermediate-depth earthquake
TL;DR: In this paper, the authors used a waveform matching technique to systematically detect earthquakes around the main shock and found that the aftershocks outline a nearly vertical southward dipping plane, which matches well with one of the nodal planes of the main shocks.