Numerical Simulation of Earthquake Nucleation Process and Seismic Precursors on Faults

来源 :Earthquake Research in China | 被引量 : 0次 | 上传用户:cheng2008YING
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To understand precursory phenomena before seismic fault sliP,this work focuses onearthquake nucleation process on a fault plane through numerical simulation.Rate and statedependent friction law with variable normal stress is employed in the analysis.The resultsshow that in the late stage of nucleation process:(1)The maximum slip velocity ismonotonically accelerating;(2)The slipping hot spot(where the slip rate is maximum)migrates spontaneously from a certain instant,and such migration is spatially continuous;(3)When the maximum velocity reaches a detectable order of magnitude(at least one orderof magnitude greater than the loading rate),the remaining time is 20 hours or longer,andthe temporal variation of slip velocity beyond this point may be used as a precursoryindicator;(4)The average slip velocity is related to the remaining time by a log-log linearrelation,which means that a similar relation between rate of microseismicity and remainingtime may also exist;(5)when normal stress variation is taken int To understand precursory phenomena before seismic fault sliP, this work focused on seismic fault sliP, this work focused on seismic fault sliP, this work focused on seismic fault sliP, this work focused on seismic fault sliP, this work focused on seismic fault sliP, this work focused on seismic fault sliP, 1) The maximum slip velocity is monotonically accelerating; (2) The slipping hot spot (where the slip rate is maximum) migrates spontaneously from a certain instant, and such migration is spatially continuous; (3) When the maximum velocity reaches a detectable order of magnitude (at least one order of magnitude greater than the loading rate), the remaining time is 20 hours or longer, and the temporal variation of slip velocity beyond this point may be used as a precursoryindicator; (4) The average slip velocity is related to the remaining time by a log-log linear relationship, which means that a similar relation between rate of microseismicity and remaining time may also exist; (5) when normal stress var iation is taken int
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