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Thomas H W Goebel1, Valerian Schuster2, Grzegorz Kwiatek2

  • 1University of Memphis, Center for Earthquake Research and Information, Memphis, TN, USA. thgoebel@memphis.edu.

PubMed
概括

由于高流体压力和低断层异质性,岩活动的持续时间会缩短. 这导致了更快的滑动加速和更少,更像地震的声学排放,特别是在未成熟的断层上.