报告地点:教学行政楼706会议室
报告时间:星期三,2015-11-04 10:00 - 11:30
报告人:佟啸鹏
报告人简介:
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报告题目:Is there a discrepancy between geological and geodetic fault slip rates?
Previous inversions for slip rate along the San Andreas Fault System (SAFS), based on elastic half-space models, show a discrepancy between the geologic and geodetic slip rates along a few major fault segments. In this study, we use an earthquake cycle model representing an elastic plate over a viscoelastic half-space to demonstrate that there is no significant discrepancy between long-term geologic and geodetic slip rates. The California statewide model includes 41 major fault segments having steady slip from the base of the locked zone to the base of the elastic plate and episodic shallow slip based on known historical ruptures and geologic recurrence intervals.