新疆克孜尔水库F_2断层近期形变特征初探
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摘要
通过对布设在克孜尔水库大坝及库区一等水准点及 GPS监测网多期观测结果的分析 ,对贯穿大坝的 F2 断层近期形变特征进行了初步研究。结果表明 :F2 断层的活动属于新构造继承性运动 ,其水平形变速率大于垂直形变速率 ,并与地震活动存在着一定相关性
Based on the several stages of results observed at the first order leveling points and GPS stations located in the dam and storage area of Kizil Reservoir, the authors primarily studied the recent deformation characteristics of fault F\-2 crossing the dam. The result shows that the activity of fault F\-2 is one kind of Neotectonic movement, and the horizontal deformation rate is more than that of vertical deformation, and which is related with the seismicity in the area.
引文
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    [3 ]杨又陵 ,杨欣 .新疆克孜尔震群活动与水库蓄水关系研究 [J].内陆地震 ,1 996,1 0 (2 ) :1 4 7~ 1 53 .
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    [5]王晓强 .北天山地震带的地壳形变过程特征及其与地震活动的关系 [J].内陆地震 ,1 987,1 (4 ) :3 86~ 3 95

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