Slow Earthquakes and Nonvolcanic Tremor

DOI Web Site 被引用文献72件
  • Gregory C. Beroza
    Department of Geophysics, Stanford University, Stanford, California 94305;
  • Satoshi Ide
    Department of Earth and Planetary Science, University of Tokyo, Bunkyo, Tokyo 113-0033, Japan;

書誌事項

公開日
2011-05-30
DOI
  • 10.1146/annurev-earth-040809-152531
公開者
Annual Reviews

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説明

<jats:p> Nonvolcanic tremor is observed in close association with geodetically observed slow-slip events in subduction zones. Accumulating evidence points to these events as members of a family of slow earthquakes that occur as shear slip on the downdip extensions of fault zones in a regime that is transitional between a frictionally locked region above and a freely slipping region below. By virtue of their locations and their properties, slow earthquakes are certain to provide new insights into the behavior of earthquakes and faulting and into the hazard they embody. </jats:p>

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