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Rheological separation of the megathrust seismogenic zone and episodic tremor and slip

Author

Listed:
  • Xiang Gao

    (Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences
    Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology)

  • Kelin Wang

    (Pacific Geoscience Centre, Geological Survey of Canada, Natural Resources Canada
    School of Earth and Ocean Sciences, University of Victoria)

Abstract

A model of the conditions required for episodic tremor and accompanying slow slip to occur, near the megathrust seismogenic zone, reconciles seemingly contradictory observations.

Suggested Citation

  • Xiang Gao & Kelin Wang, 2017. "Rheological separation of the megathrust seismogenic zone and episodic tremor and slip," Nature, Nature, vol. 543(7645), pages 416-419, March.
    • Handle: RePEc:nat:nature:v:543:y:2017:i:7645:d:10.1038_nature21389
    DOI: 10.1038/nature21389
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    Cited by:

    1. Ryosuke Oyanagi & Atsushi Okamoto, 2024. "Subducted carbon weakens the forearc mantle wedge in a warm subduction zone," Nature Communications, Nature, vol. 15(1), pages 1-9, December.

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