Applying unsupervised machine-learning algorithms and MUSIC back-projection to characterize 2018–2022 Hualien earthquake sequence
The city of Hualien in eastern Taiwan is located at the junction of the Luzon arc–Eurasian continent collision and the oblique subduction of the Philippine Sea plate along the Ryukyu Trench. This complex tectonic setting creates one of the most intense seismic hazards in the world. Since the mid-twe...
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| Published in: | TAO : Terrestrial, atmospheric, and oceanic sciences Vol. 33; no. 1; pp. 1 - 18 |
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| Main Authors: | , |
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| Language: | English |
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Springer Nature Singapore
01.12.2022
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| ISSN: | 1017-0839, 2311-7680 |
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| Abstract | The city of Hualien in eastern Taiwan is located at the junction of the Luzon arc–Eurasian continent collision and the oblique subduction of the Philippine Sea plate along the Ryukyu Trench. This complex tectonic setting creates one of the most intense seismic hazards in the world. Since the mid-twentieth century, three earthquake sequences (1951, 1986–1992, and 2018–2022) have caused severe damages and revealed a diversity of focal mechanisms, demonstrating a complex seismogenic tectonic interactions of collisions and subductions. In this study, we used the two-dimensional back-projection method to examine rupture characteristics of three strong earthquakes during the latest sequence (2018–2022). We also studied the same earthquake sequence using unsupervised machine-learning via density-based spatial clustering of applications with noise (DBSCAN) and principal component analysis (PCA). Our results revealed two westward dipping seismogenic structures. The deeper one lies beneath the eastern flank of the Central Range and the shallower one rotates clockwise along the coastline from south to north. Overall, focal mechanisms within these two structures are consistent with planar geometries obtained using PCA. The deeper structure beneath the Central Range is likely an imbricated fault system. The coastline structure is characterized by a transition of strike and dip angles from south to north. We suggest that the subhorizontal nodal planes in earthquakes offshore Hualien are related to the shallow northward dipping patch in the northern part of the coastal structure. Our Coulomb stress change results revealed strong linkages between these two structures.
Key points
We used unsupervised machine-learning algorithms DBSCAN and PCA to study the 2018–2022 Hualien earthquake sequence.
A deep westward-dipping and a shallow rotation structure system are revealed from earthquake clusters close to the northernmost Longitudinal Valley.
Coulomb stress change is used to ascertain cascaded triggering on these two structures. |
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| AbstractList | The city of Hualien in eastern Taiwan is located at the junction of the Luzon arc–Eurasian continent collision and the oblique subduction of the Philippine Sea plate along the Ryukyu Trench. This complex tectonic setting creates one of the most intense seismic hazards in the world. Since the mid-twentieth century, three earthquake sequences (1951, 1986–1992, and 2018–2022) have caused severe damages and revealed a diversity of focal mechanisms, demonstrating a complex seismogenic tectonic interactions of collisions and subductions. In this study, we used the two-dimensional back-projection method to examine rupture characteristics of three strong earthquakes during the latest sequence (2018–2022). We also studied the same earthquake sequence using unsupervised machine-learning via density-based spatial clustering of applications with noise (DBSCAN) and principal component analysis (PCA). Our results revealed two westward dipping seismogenic structures. The deeper one lies beneath the eastern flank of the Central Range and the shallower one rotates clockwise along the coastline from south to north. Overall, focal mechanisms within these two structures are consistent with planar geometries obtained using PCA. The deeper structure beneath the Central Range is likely an imbricated fault system. The coastline structure is characterized by a transition of strike and dip angles from south to north. We suggest that the subhorizontal nodal planes in earthquakes offshore Hualien are related to the shallow northward dipping patch in the northern part of the coastal structure. Our Coulomb stress change results revealed strong linkages between these two structures. Key points 1. We used unsupervised machine-learning algorithms DBSCAN and PCA to study the 2018–2022 Hualien earthquake sequence. 2. A deep westward-dipping and a shallow rotation structure system are revealed from earthquake clusters close to the northernmost Longitudinal Valley. 3. Coulomb stress change is used to ascertain cascaded triggering on these two structures. The city of Hualien in eastern Taiwan is located at the junction of the Luzon arc–Eurasian continent collision and the oblique subduction of the Philippine Sea plate along the Ryukyu Trench. This complex tectonic setting creates one of the most intense seismic hazards in the world. Since the mid-twentieth century, three earthquake sequences (1951, 1986–1992, and 2018–2022) have caused severe damages and revealed a diversity of focal mechanisms, demonstrating a complex seismogenic tectonic interactions of collisions and subductions. In this study, we used the two-dimensional back-projection method to examine rupture characteristics of three strong earthquakes during the latest sequence (2018–2022). We also studied the same earthquake sequence using unsupervised machine-learning via density-based spatial clustering of applications with noise (DBSCAN) and principal component analysis (PCA). Our results revealed two westward dipping seismogenic structures. The deeper one lies beneath the eastern flank of the Central Range and the shallower one rotates clockwise along the coastline from south to north. Overall, focal mechanisms within these two structures are consistent with planar geometries obtained using PCA. The deeper structure beneath the Central Range is likely an imbricated fault system. The coastline structure is characterized by a transition of strike and dip angles from south to north. We suggest that the subhorizontal nodal planes in earthquakes offshore Hualien are related to the shallow northward dipping patch in the northern part of the coastal structure. Our Coulomb stress change results revealed strong linkages between these two structures. Key points We used unsupervised machine-learning algorithms DBSCAN and PCA to study the 2018–2022 Hualien earthquake sequence. A deep westward-dipping and a shallow rotation structure system are revealed from earthquake clusters close to the northernmost Longitudinal Valley. Coulomb stress change is used to ascertain cascaded triggering on these two structures. |
| ArticleNumber | 28 |
| Author | Wang, Yu Jian, Pei-Ru |
| Author_xml | – sequence: 1 givenname: Pei-Ru orcidid: 0000-0003-3221-0291 surname: Jian fullname: Jian, Pei-Ru email: prjian@earth.sinica.edu.tw organization: Institute of Earth Sciences, Academia Sinica – sequence: 2 givenname: Yu orcidid: 0000-0001-6798-2721 surname: Wang fullname: Wang, Yu email: wangyu79@ntu.edu.tw organization: Department of Geosciences, National Taiwan University |
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| Cites_doi | 10.1002/2016GL071128 10.1130/0091-7613(2002)030<0935:adotib>2.0.co;2 10.1002/2017GL075724 10.1016/0031-9201(85)90011-1 10.1029/1999tc900055 10.1016/j.neucom.2017.01.026 10.1785/0220180227 10.3319/TAO.2020.06.08.01 10.1029/2004jb003251 10.1785/0220180182 10.1002/2017gl072552 10.1016/j.epsl.2014.02.026 10.1029/97jb03510 10.3319/tao.2001.12.s.209(odp) 10.1146/annurev.earth.33.092203.122505 10.3319/TAO.2018.12.09.03 10.1016/0040-1951(87)90020-5 10.1016/j.tecto.2016.03.038 10.1785/0220180228 10.1029/2004JB003415 10.1038/nature03675 10.1130/G21834.1 10.1785/0120070115 10.1785/0120170231 10.1016/j.tecto.2013.03.020 10.1029/2011gc003751 10.1029/92jb00132 10.1016/s0040-1951(00)00272-9 10.1029/2007JB005414 10.1785/0120000006 10.1029/2007JB004983 10.1016/j.epsl.2005.01.018 10.1016/j.epsl.2004.10.031 10.1029/2010JB007831 10.1016/0040-1951(90)90188-e 10.1029/2002JB001764 10.1785/0220180241 10.1785/0120070166 10.5047/eps.2012.05.010 10.3319/tao.2013.12.25.01(tt) 10.3319/tao.2004.15.1.61(T) 10.1098/rsta.2015.0202 10.1029/2011GL048118 10.1785/0120090189 10.1002/2017JB015021 10.1016/0012-821x(94)90085-x 10.1016/j.epsl.2008.02.035 10.1177/0025802419893168 10.1785/0120100223 10.1111/j.1365-246X.2010.04813.x 10.1029/2011GL049223 10.1002/jgrb.50179 10.1029/2007JB005048 10.3319/tao.2015.11.27.02(TEM) 10.1007/s44195-022-00017-z 10.3319/TAO.2018.12.23.01 10.1109/ICDMW.2008.119 10.1007/978-3-540-88558-0_8 10.1117/12.2181526 10.3133/ofr7541 10.1029/2022JB024054 |
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| Snippet | The city of Hualien in eastern Taiwan is located at the junction of the Luzon arc–Eurasian continent collision and the oblique subduction of the Philippine Sea... Key points 1. We used unsupervised machine-learning algorithms DBSCAN and PCA to study the 2018–2022 Hualien earthquake sequence. 2. A deep westward-dipping... |
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| SubjectTerms | Atmospheric Sciences Central Range fault Coastal rotation structure DBSCAN Earth and Environmental Science Earth Sciences Hualien earthquakes Oceanography Original Article PCA Unsupervised machine learning |
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| Title | Applying unsupervised machine-learning algorithms and MUSIC back-projection to characterize 2018–2022 Hualien earthquake sequence |
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