Origin of High‐Frequency Radiation During Laboratory Earthquakes-Reference-Cited by-同舟云学术

Origin of High‐Frequency Radiation During Laboratory Earthquakes

Published:2019-04-15 Issue:7 Volume:46 Page:3755-3763
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Marty S.¹^ORCID,Passelègue F. X.²,Aubry J.¹^ORCID,Bhat H. S.¹,Schubnel A.¹,Madariaga R.¹^ORCID

Affiliation:

1. Laboratoire de Géologie, École Normale Supérieure/CNRS UMR 8538PSL Research University Paris France

2. École Polytechnique Fédérale de Lausanne Lausanne Switzerland

Funder

FP7 Ideas: European Research Council

European Research Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080519

Reference44 articles.

1. Scaling law of seismic spectrum

2. Rupture velocity of plane strain shear cracks

3. Frictional Heating Processes and Energy Budget During Laboratory Earthquakes

4. High-frequency seismic radiation from a buried circular fault

5. Off‐fault damage patterns due to supershear ruptures with application to the 2001 Mw 8.1 Kokoxili (Kunlun) Tibet earthquake;Bhat H. S.;Journal of Geophysical Research,2007

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