作者:Feng Hu,Hanqing Huang,Xiaofei Chen
摘要:Based on dynamic rupture simulations on a planar fault in a homogeneous half-space, we investigated the nucleation processes using the time-weakening friction law. Both the characteristic time and the rupture speed in the nucleation asperity play an important role in determining rupture behaviors on a fault plane following the time-weakening friction law, with which rupture starts from a single point in the nucleation asperity and propagates at a given speed toward the boundary of the nucleation area. Rupture with a small characteristic time or a large rupture speed in the nucleation asperity propagates earlier from the hypocenter. Rupture following the slipweakening friction law requires a smaller radius of nucleation patch to have similar rupture front contours of the time-weakening friction law. Even if the rupture velocity in the nucleation patch of the time-weakening friction law increases to infinity, the peak slip rate in the nucleation asperity is smaller than that of the slip-weakening law. The peak ground velocity distributions of ruptures following the two friction laws are also compared.
發文機構:Laboratory of Seismology and Physics of Earth's Interior andSchool of Earth and Space Sciences Department of Earth and Space Science
關鍵詞:摩擦定律利用時間成核過程弱化動態斷裂特征時間峰值分布大破裂Time-weakening friction law Slip-weakening friction law Dynamic rupture Ground motion
分類號: O313.5[理學—一般力學與力學基礎][理學—力學]S834.4[農業科學—畜牧學][農業科學—畜牧獸醫]