Teleseismic Waveform Complexities Caused by Near Trench Structures and Their Impacts on Earthquake Source Study: Application to the 2015 Illapel Aftershocks (Central Chile)-Reference-Cited by-同舟云学术

Teleseismic Waveform Complexities Caused by Near Trench Structures and Their Impacts on Earthquake Source Study: Application to the 2015 Illapel Aftershocks (Central Chile)

Published:2019-01 Issue:1 Volume:124 Page:870-889
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Qian Yunyi¹²³,Wei Shengji¹⁴^ORCID,Wu Wenbo⁵,Zeng Hongyu¹,Coudurier‐Curveur Aurélie¹^ORCID,Ni Sidao⁶^ORCID

Affiliation:

1. Earth Observatory of SingaporeNanyang Technological University Singapore

2. School of Earth and Space SciencesUniversity of Science and Technology of China Hefei China

3. Department of Earth and Space SciencesSouthern University of Science and Technology Shenzhen China

4. Asian School of the EnvironmentNanyang Technological University Singapore

5. Department of GeosciencesPrinceton University Princeton NJ USA

6. State Key Laboratory of Geodesy and Earth's DynamicsInstitute of Geodesy and Geophysics Wuhan China

Funder

Ministry of Education - Singapore

National Research Foundation Singapore

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016143

Reference47 articles.

1. The 2015 Mw 8.3 Illapel, Chile, Earthquake: Direction‐Reversed Along‐Dip Rupture with Localized Water Reverberation

2. Episodic development of a convergent margin inferred from structures and processes along the southern Chile margin

3. Gravity anomalies, crustal structure, and seismicity at subduction zones: 1. Seafloor roughness and subducting relief

4. An updated digital model of plate boundaries

5. CAPjoint, A Computer Software Package for Joint Inversion of Moderate Earthquake Source Parameters with Local and Teleseismic Waveforms

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