Revealing the cluster of slow transients behind a large slow slip event-Reference-Cited by-同舟云学术

Revealing the cluster of slow transients behind a large slow slip event

Author:

Frank William B.¹^ORCID,Rousset Baptiste²,Lasserre Cécile³,Campillo Michel¹⁴

Affiliation:

1. Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139–4307, USA.

2. Department of Earth and Planetary Sciences, University of California, Berkeley, Berkeley, CA 94720–4767, USA.

3. Université de Lyon, UCBL, ENSL, CNRS, LGL-TPE, Villeurbanne, France.

4. Institut des Sciences de la Terre, Université Grenoble Alpes, CNRS, IRD, Saint-Martin-d’Hères, France.

Abstract

A slow slip event is a cluster of small aseismic slip transients intermittently interrupted by relocking of the plate interface.

Funder

National Science Foundation

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference50 articles.

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