民乐-山丹6.1级地震前后的地壳垂直形变
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摘要
利用青藏块体东北部的区域水准、跨断裂水准和断层形变资料,分析了2003年10月25日民乐-山丹6.1级地震前后的地壳垂直形变。结果表明,震前出现了明显的长、中、短期形变前兆异常。在经历了1995~2000年的缓慢形变阶段后,2000~2002年祁连山断裂带中、西段形变显著加速,2003年3~10月断层形变异常数量经历了一个“少-多-少”的演变过程,并沿构造体自外围向震中附近收缩;震后祁连山断裂带中、西段形变反向,东段则出现局部隆起区。
Using observations of regional leveling, cross-faults leveling and fault deformation in the northern Qinghai-Tibet block, the vertical crust deformation before and after Minle-Shandan Ms6.1 earthquake on October 25, 2003 is analyzed. The results show that: there are obvious anomalous characteristics in long-medium-term and short-impending stage before earthquake;after slower deformation stage from 1995 to 2000, the deformation accelerated in middle and west part of Qilian fault zone from 2000 to 2002,the quantity of anomalies had gone through a evolutive process of “small-large-small” from March to October in 2003,and the fault deformation anomaly has the characteristic that it contracts from the outside to the source region.After the event there has been the contrary deformation in the middle and the west part of Qilian fault zone and a rise region appears in the east segment.
引文
[1]甘肃省地震局.甘肃省地震局2000年年中震情趋势研究报告.2000.
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