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滇池盆地东缘白邑-横冲断裂南段的浅层地震勘探研究

Exploration of Southern Segment of Baiyi-Henchong Fault in the Eastern Dianchi Basin Using Shallow Seismic Survey

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【作者】 胡毅力温一波段继平太树刚王刚李建有王朝进杨江华

【Author】 Hu Yili1),Wen Yibo2),Duan Jiping3),Tai Shugang3),Wang Gang3), Li Jianyou3),Wang Chaojin3) and Yang Jianghua3) 1) Department of Geophysics,Yunnan University,Kunming 650091,China 2) College of City Construction and Management,Yunnan University,Kunming 650091,China 3) Kunming Southern Geophysical Technology Development,Inc.,Kunming 650223,China

【机构】 云南大学地球物理系云南大学城建学院昆明南方地球物理技术开发有限公司

【摘要】 本文用浅层地震反射波法对可能穿越昆明新城区东部第四系覆盖区的白邑-横冲断裂南段进行了探测,结果表明:采用浅层地震反射波法探测隐伏断层是有效的,在滇池盆地东缘,白邑-横冲断裂南段东支在隐伏区存在,断面接近直立,视倾角约80°,具有高倾角张性正断性质,基岩垂直错距为10—13m,断裂规模由北向南减小;同时,没有发现西支次级断层存在迹象。据土层测龄结果,东支断裂最新活动时代为第四纪中更新世晚期。

【Abstract】 The shallow seismic reflection exploration is applied to explore the buried southern segment of Baiyi-Henchong fault which is located in the east of New City of Kunming.The exploration reveals that the fault plane is nearly vertical,and the apparent dip is about 80°degree.The vertical displacement is between 10 to 13 meters,and the size of fault becomes smaller from the north to the south.The fault is characterized with a normal tensile fault with high dip angle.No evidence of secondary fault was detected in this survey.The results from dating of soil samples indicate the last faulting activity occurred in the late period of middle Pleistocene.

【基金】 云南省自然科学基金(2007DOBM)资助
  • 【文献出处】 震灾防御技术 ,Technology for Earthquake Disaster Prevention , 编辑部邮箱 ,2010年04期
  • 【分类号】P631.4
  • 【被引频次】3
  • 【下载频次】66
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