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浅层地震剖面揭示固原市清水河东侧断裂特征
Characteristics of the Qingshui River East Fault in Guyuan City as Revealed by Shallow Seismic Profiles
【摘要】 为查明清水河东侧断裂的产状、性质及其浅部构造特征,跨断裂开展高分辨率的浅层地震探测,获得高信噪比的浅层地震反射叠加剖面。根据浅层地震剖面结果并结合该区域地质资料,对该断裂的浅部构造特征进行分析和讨论。结果表明,清水河东侧断裂为一条走向近SN、倾向E的逆断层,其浅部为由2~3条断层组成的"Y"字形构造,并错断埋深约10~30 m的第四系沉积层,属第四纪以来的隐伏活动断裂。
【Abstract】 In order to investigate the occurrences, properties and shallow tectonic features of the east-Qingshui river fault, we complete high resolution shallow seismic profiles crossing the fault and obtain shallow seismic reflection stacked profiles which have higher signal-noise ratio. According to these results, and combined with geological data, we analyze and discuss the shallow structures features of the fault. The results show that east-Qingshui river fault is a near SN trending and E dipping reverse fault. In the shallow position the east-Qingshui river, the fault shows "Y" structure which consists of 2-3 fault. The fault disrupts 10~20 m Quaternary strata in the shallow part, therefore it buried active faults in the Quaternary period.
【Key words】 Guyuan city; active fault exploration; shallow seismic reflection profile; east-Qingshui river fault;
- 【文献出处】 大地测量与地球动力学 ,Journal of Geodesy and Geodynamics , 编辑部邮箱 ,2019年08期
- 【分类号】P631.4
- 【被引频次】1
- 【下载频次】127