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- W3150291170 abstract "在 Wenchuan 地震以后的 Yingxiu-Beichuan 差错的今日的压力状态被重新估计使用在原处测量了在 Wenchuan 地震以后获得的压力数据。结果表明主要压力对深度的坡度系数沿着 Yingxiu-Beichuan 差错从南方减少到北方，表明压力铺平到北方的来自南方的减少。在在地震期间产生的今日的压力层次和表面破裂之间的一致性显示在在 Wenchuan 地震前的 Yingxiu-Beichuan 差错下面的积累的构造压力被减轻处于良好的竟技状态表面破裂。这导致了在 Yingxiu-Beichuan 差错，但是相对的南部的节仍然保持高的压力在北节低。反常高毛孔压力条件和一个极其低的摩擦系数在沿着这个差错在 Wenchuan 地震以后观察的压力地调整和地震事件的解释起重要作用，根据用合并从 0.4 ～ 1.0 的摩擦系数的库仑摩擦失败的理论的评价结果。为了精确地由分析估计 Yingxiu-Beichuan 差错的地震学上的危险，用库仑摩擦失败的理论指责不稳定性，许多注意应该在今日的压力状态下面集中于毛孔压力条件和摩擦系数的进化状态。" @default.
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- W3150291170 date "2016-01-01" @default.
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- W3150291170 title "Reexamining the Seismological Implications of the Present-day Stress State of the Yingxiu-Beichuan Fault after the Wenchuan Earthquake" @default.
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