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成都平原隐伏断层氡气特征及断层活动性判别
引用本文:文龙,梁斌,王全伟,朱兵,付小方,应立朝,王鑫,徐永胜.成都平原隐伏断层氡气特征及断层活动性判别[J].四川地质学报,2013(3):257-261.
作者姓名:文龙  梁斌  王全伟  朱兵  付小方  应立朝  王鑫  徐永胜
作者单位:[1]西南科技大学环境与资源学院,四川绵阳621010 [2]四川省地质调查院,成都610081
基金项目:基金项目:中国地质调查局1:25万成都幅区域地质调查项目(项目编号:1212010880704);四川省国土资源厅重点项目(批准号:KJ-2010-5)资助
摘    要:对成都平原8条具有代表性的隐伏断层进行氡气测量,其研究表明其氡气特征除新津断层外其余都表现为多峰异常,成都平原隐伏断层大多为规模较大的断裂带,可能有多个分支断层组成。位于成都平原中西部边缘的隐伏断层活动性强于东部的隐伏断层,表明成都平原隐伏断层活动性受龙门山构造的控制。通过该研究,为监测隐伏断层的地震活动性提供了新的途径。

关 键 词:隐伏断层  氡气  活动性  成都平原

Radon Survey and Fault Activity in Buried Faults on the Chengdu Plain
WEN Long,LIANG Bi,WANG Quan-wei,ZHU Bing,FU Xiao-fang,YING Li-chao,WANG Xin,XU Yong-sheng.Radon Survey and Fault Activity in Buried Faults on the Chengdu Plain[J].Acta Geologica Sichuan,2013(3):257-261.
Authors:WEN Long  LIANG Bi  WANG Quan-wei  ZHU Bing  FU Xiao-fang  YING Li-chao  WANG Xin  XU Yong-sheng
Institution:1-School of Environment and Resource, Southwest University of Science and Technology, Mianyang, Sichuan 621010; 2-Sichuan Geological Survey, Chengdu 610081)
Abstract:Most of buried faults on the Chengdu Plain large fault zones composed of multiple branch faults. Radon survey on the eight buried faults on the Chengdu Plain shows multiple peak anomalies with the exception of the Xinjin fault. Activity of the buried faults on the western margin of the Chengdu Plain is stronger than the that of those in the east based on radon anomalies, which indicates that the buried faults on the Chengdu Plain were controlled by the Longmenshan tectonic zone.
Keywords:Chengdu plain  radon survey  buried fault  activity
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