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本文指出,可应用对应原理及沃尔什与赖斯的弹性解作面积分,即可算出粘弹性半空间断层活动所导致的重力变化.结果表明,重力变化并不依赖于粘弹性质,而且与滑移历史有预期不到的简单关系.
This paper points out that the change of gravity caused by the viscoelastic half-space fault activity can be calculated by applying the corresponding principle and the elastic integral area of Walsh and Rice.The results show that the change of gravity does not depend on the viscoelastic properties, Simple relationship with slippage history unexpectedly.