沂沭断裂带跨断层形变异常及其解释
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摘要
沂沭断裂带及其附近北西向断裂上存在的甘霖、五胜和高峰头流动短水准异常进行了分析,分析认为存在的3项短水准异常是汶川地震前后区域地壳应力增强引起的可能性较大。
Through analyzing the anomaly of Ganlin,Wusheng and Gaofengtou mobile short leveling in Yishu fault zone and surrounding NW strike faults and discussing the anomaly mechanism,we think that the three anomalyies are likely caused by crustal stress increasing in this area before and after Wenchuan earthquake.
引文
①李杰.沂沭断裂带及附近地区跨断层形变异常跟踪分析[R].山东省2008年度地震趋势研究报告,2007.
    ②李杰.跨断层流动短水准异常变化跟踪分析[R].山东省2009年度地震趋势研究报告,2008.
    ③李杰.山东跨断层形变异常跟踪及地震危险性分析[R].山东省2010年度地震趋势研究报告,2009.
    ④http://www.csndmc.ac.cn/newweb/catalog-direct-link.htm
    ⑤肖兰喜.山东近期跨断层短水准异常的可能物理机理[R].山东省2011年度地震趋势研究报告,2010
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