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临潼-长安断裂带主要由两条主断层和两条分支断层组成,断层基本沿北东向的黄土塬陡坎展布,陡坎高30~128m不等。虽然断层和陡坎有很好的重合关系,但陡坎并不完全是断层所形成,主要原因有:1)野外断层露头表明,断层错断S1古土壤层一般为0.2~1.5m,最大为6.0m,错断S2~S4古土壤层也仅有几米,与断层所在的陡坎高度相比,断层的错距很小;2)高桥和月登阁钻探结果显示,钻孔中早更新世地层上部断层错距分别不大于24.45m和8.49m,即断层在黄土塬基座中的错距比相应的黄土陡坎高度要小;3)在某些局部地段断层并不随陡坎拐弯而拐弯;4)深孔资料显示有侵蚀现象。综合分析,临潼-长安断裂带所在的陡坎是侵蚀作用和断层错动共同作用的结果,陡坎的形成以侵蚀作用为主,断层的错动量很小。地壳抬升、断块掀斜运动产生断层,新近纪或早更新世"三门湖"在已有的断层位置发生侵蚀,两者共同作用形成了现今地貌陡坎。 相似文献
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利用中国地壳运动观测网络工程1999~2002年渭河盆地及邻近地区GPS观测资料,以及陕西省地震局2001~2002年的GPS观测资料,研究了渭河盆地及周邻地区地壳运动速度场. 结果表明, 渭河盆地及邻区的运动速率有明显的北东向条带状变化特征,鄂尔多斯块体南缘呈整体不连续性逆时针旋转运动,相对鄂尔多斯块体内部的榆林测点,平均速率约为5.7 mm/a;渭河盆地中部的彬县——西安——蓝田一线,两侧存在一个显著的左旋剪切带,其北部区域与铜川——泾阳——临潼——渭南小震频发区有较好的对应关系. 相似文献
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The results of seismic deep reflection,high resolution refraction and shallow artificial seismic exploration indicate that the fault on the northern bank of the Weihe river is composed of two faults,one is the Yaodian-Zhangjiawan fault and the other is the Chuanzhang-Zuitou fault.The 22 km long Yaodian-Zhangjiawan fault of EW-striking starts from Chenjiagou via Yaodian town,Qianpai village,Bili village,Wujia town and Zhangjiawan to Jiajiatan.The 15 km long Chuanzhang-Zuitou fault striking near EW starts from Chuanzhang via Mabei to Zuitou.The Weihe fault offset the basement and upper crust,the reflecting layers of TQ,TN,TE and Tg are ruptured at depth of about 15 km.In the deep part,the Weihe fault and the secondary fault form a Y-shaped structure or a synthetic low angle intersection.The Weihe fault is a listric normal fault.The fault has obvious structural characteristics of a reversed-drag normal fault and a normal drag normal fault with the depth of 1 000 m,and also has the characteris-tics of syngenetic sediment.The Weihe fault is one of the faults which control the basin sediment,and it is the boundary fault of Xi’an depression and Xianyang salient.The depth of the fault decreases from the west to east gradually,the deep part intersects with the Lintong-Chang’an fault at the intersection part of Weihe River,Jinghe River and Bahe River and the shallow part connects with the Weinan-Jingyang fault.The seismic exploration re-sults indicate that no fault exists on southern bank of the Weihe River. 相似文献
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