Improved understanding of earthquake interaction with waveform matching method

As one of the most common geological phenomena, earthquake occurs in various tectonic settings, such as fault zone along plate boundaries, volcanoes, and oil/gas production sites. The stress changes caused by large earthquake are capable of triggering new seismicity from near-field to far-field. Bet...

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Bibliographic Details
Main Author: Li, Chenyu
Other Authors: Peng, Zhigang, Earth and Atmospheric Sciences, Newman, Andrew V., McClellan, James H., Herrmann, Felix, Dai, Sheng
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Georgia Institute of Technology 2020
Subjects:
Online Access:http://hdl.handle.net/1853/63694
id ftgeorgiatech:oai:smartech.gatech.edu:1853/63694
record_format openpolar
spelling ftgeorgiatech:oai:smartech.gatech.edu:1853/63694 2023-05-15T14:01:30+02:00 Improved understanding of earthquake interaction with waveform matching method Li, Chenyu Peng, Zhigang Earth and Atmospheric Sciences Newman, Andrew V. McClellan, James H. Herrmann, Felix Dai, Sheng 2020-09-08T12:49:00Z application/pdf http://hdl.handle.net/1853/63694 en_US eng Georgia Institute of Technology http://hdl.handle.net/1853/63694 Earthquake triggering Earthquake detection Text Dissertation 2020 ftgeorgiatech 2023-01-30T18:42:49Z As one of the most common geological phenomena, earthquake occurs in various tectonic settings, such as fault zone along plate boundaries, volcanoes, and oil/gas production sites. The stress changes caused by large earthquake are capable of triggering new seismicity from near-field to far-field. Better understanding of the interaction mechanism among diverse seismic events is significant to learn about the fundamental fault behaviors as well as mitigate potential seismic-related hazards. In order to do so, detailed seismicity documentation and analysis are essential. Traditional earthquake catalogs adopted by analysts and automatic algorithms based on signal-to-noise ratio (SNR) tend to miss weak events buried in the coda wave of large earthquake or noises. In this study, a semi-automatic template-matching earthquake detection method is utilized, which cross-correlates waveform of known events with continuous data for new event recognition. Specifically, we use this method to study dynamic triggered earthquakes in volcanoes (Changbaishan in China and Mt. Erebus in Antarctica) and geothermal regions (Salton Sea Geothermal Field). The behaviors of dynamic triggering in these regions have both similarities and different site-dependent responses. The template matching is also applied to aftershock sequence of the 2015 Mw7.5 Hindu Kush intermediate-depth earthquake, consequently more than 14 times events are detected compared to the listed ones in the standard catalog. This result strongly demonstrates the potential to further expand deep earthquake catalog with template matching method. Finally, we explore two recently-developed seismic event detection methods, one is network based waveform-similarity method for large-N array, and another is based on CNN. They offer more opportunities to automatically detect seismicity in regions with deficient catalog events. Ph.D. Doctoral or Postdoctoral Thesis Antarc* Antarctica Georgia Institute of Technology: SMARTech - Scholarly Materials and Research at Georgia Tech
institution Open Polar
collection Georgia Institute of Technology: SMARTech - Scholarly Materials and Research at Georgia Tech
op_collection_id ftgeorgiatech
language English
topic Earthquake triggering
Earthquake detection
spellingShingle Earthquake triggering
Earthquake detection
Li, Chenyu
Improved understanding of earthquake interaction with waveform matching method
topic_facet Earthquake triggering
Earthquake detection
description As one of the most common geological phenomena, earthquake occurs in various tectonic settings, such as fault zone along plate boundaries, volcanoes, and oil/gas production sites. The stress changes caused by large earthquake are capable of triggering new seismicity from near-field to far-field. Better understanding of the interaction mechanism among diverse seismic events is significant to learn about the fundamental fault behaviors as well as mitigate potential seismic-related hazards. In order to do so, detailed seismicity documentation and analysis are essential. Traditional earthquake catalogs adopted by analysts and automatic algorithms based on signal-to-noise ratio (SNR) tend to miss weak events buried in the coda wave of large earthquake or noises. In this study, a semi-automatic template-matching earthquake detection method is utilized, which cross-correlates waveform of known events with continuous data for new event recognition. Specifically, we use this method to study dynamic triggered earthquakes in volcanoes (Changbaishan in China and Mt. Erebus in Antarctica) and geothermal regions (Salton Sea Geothermal Field). The behaviors of dynamic triggering in these regions have both similarities and different site-dependent responses. The template matching is also applied to aftershock sequence of the 2015 Mw7.5 Hindu Kush intermediate-depth earthquake, consequently more than 14 times events are detected compared to the listed ones in the standard catalog. This result strongly demonstrates the potential to further expand deep earthquake catalog with template matching method. Finally, we explore two recently-developed seismic event detection methods, one is network based waveform-similarity method for large-N array, and another is based on CNN. They offer more opportunities to automatically detect seismicity in regions with deficient catalog events. Ph.D.
author2 Peng, Zhigang
Earth and Atmospheric Sciences
Newman, Andrew V.
McClellan, James H.
Herrmann, Felix
Dai, Sheng
format Doctoral or Postdoctoral Thesis
author Li, Chenyu
author_facet Li, Chenyu
author_sort Li, Chenyu
title Improved understanding of earthquake interaction with waveform matching method
title_short Improved understanding of earthquake interaction with waveform matching method
title_full Improved understanding of earthquake interaction with waveform matching method
title_fullStr Improved understanding of earthquake interaction with waveform matching method
title_full_unstemmed Improved understanding of earthquake interaction with waveform matching method
title_sort improved understanding of earthquake interaction with waveform matching method
publisher Georgia Institute of Technology
publishDate 2020
url http://hdl.handle.net/1853/63694
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation http://hdl.handle.net/1853/63694
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