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ABSTRACT:
SUBMITTER: Rousset B
PROVIDER: S-EPMC6374109 | biostudies-literature | 2019 Feb
REPOSITORIES: biostudies-literature
Rousset Baptiste B Bürgmann Roland R Campillo Michel M
Science advances 20190213 2
Episodic tremor and accompanying slow slip are observed at the down-dip edge of subduction seismogenic zones. While tremors are the seismic signature of this phenomenon, they correspond to a small fraction of the moment released; thus, the associated fault slip can be quantified only by geodetic observations. On continental strike-slip faults, tremors have been observed in the roots of the Parkfield segment of the San Andreas fault. However, associated transient aseismic slip has never been dete ...[more]