【摘要】 台湾南投大震是震源地方一个逆掩断层错动引起的 ,上盘向西错动 ,这种断层错动的形式其 Corioli力效应是使两断层盘相互挤压 ,因之主震发生时能量释放不彻底 ,余震强度较大。本文试图用 Corioli力效应具体讨论台湾南投大震的余震强度更多还原

【Abstract】 The Natou great earthquake in the Taiwan island is caused by a dislocation of thrust in the source region with its upper wall slipping toward the west The Corioli force of this type of dislocation makes both of fault walls compress each other Therefore, the total energy does not release completely during the mainshock and the magnitudes of the aftershocks are very large An attempt to analyze the effect of Corioli force on the aftershock intentisity of the Natou great earthquake is made in this paper更多还原