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地震学报

81地震北向重力梯度同震变化的可能性进行分析. 研究结果表明 在尼泊尔. 81地震发生前北向重力梯度表现出比较明显的正负异常变化而该地震即发生在北向重力梯度正负变化的零值线附近 研究区北向重力梯度年变率在印度板块边界及其垂直方向所形成的四象限呈正负相间分布6个特征点的北向重力梯度在2012年4月出现比较明显的跳变. 由此推断北向重力梯度的动态变化过程反映了震前区域物质迁移和震后壳幔物质黏滞性调整等问题. 为了深入认识2016年4月15日日本熊本地震破裂的复杂性利用远场体波资料和同震InSAR资料联合反演了此次地震的震源破裂时空过程. 联合反演结果表明 熊本地震的震源破裂持续时间约为25 s整个破裂过程释放的总标量矩为6.03 10. Doi 10.11939jass.20170077. Doi 10.11939jass.20170209. Doi 10.11939jass.20170215. 结果显示 在芦山地震发生之前汶川地震余震的应力降随时间的增加而逐渐增大 在芦山地震发生之后龙门山断裂上余震的应力降明显下降并在之后随着时间缓慢增大 部分 M. Doi 10.1.
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地震学报

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81地震北向重力梯度同震变化的可能性进行分析. 研究结果表明 在尼泊尔. 81地震发生前北向重力梯度表现出比较明显的正负异常变化而该地震即发生在北向重力梯度正负变化的零值线附近 研究区北向重力梯度年变率在印度板块边界及其垂直方向所形成的四象限呈正负相间分布6个特征点的北向重力梯度在2012年4月出现比较明显的跳变. 由此推断北向重力梯度的动态变化过程反映了震前区域物质迁移和震后壳幔物质黏滞性调整等问题. 为了深入认识2016年4月15日日本熊本地震破裂的复杂性利用远场体波资料和同震InSAR资料联合反演了此次地震的震源破裂时空过程. 联合反演结果表明 熊本地震的震源破裂持续时间约为25 s整个破裂过程释放的总标量矩为6.03 10. Doi 10.11939jass.20170077. Doi 10.11939jass.20170209. Doi 10.11939jass.20170215. 结果显示 在芦山地震发生之前汶川地震余震的应力降随时间的增加而逐渐增大 在芦山地震发生之后龙门山断裂上余震的应力降明显下降并在之后随着时间缓慢增大 部分 M. Doi 10.1.

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This web page dzxb.org states the following, "结果显示 在芦山地震发生之前汶川地震余震的应力降随时间的增加而逐渐增大 在芦山地震发生之后龙门山断裂上余震的应力降明显下降并在之后随着时间缓慢增大 部分 M."

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