首页 | 本学科首页   官方微博 | 高级检索  
     检索      

三河-平谷活断层汞地球化学特征
引用本文:王传远,杜建国,周晓成.三河-平谷活断层汞地球化学特征[J].地震,2004,24(1):132-136.
作者姓名:王传远  杜建国  周晓成
作者单位:中国地震局分析预报中心, 北京 100036
基金项目:国家重大基金项目(12099040)
摘    要:应用QM201G便携式测汞仪在河北省潘各庄进行野外现场勘测, 研究了三河-平谷活断层汞地球化学特征, 确定了该区段断层的具体位置。 测区土壤中气态汞浓度为0.001~0.246 ng/L, 背景值为0.015 ng/L。 在断裂破碎带的土壤中气态汞含量高出背景值十多倍。 地震断裂带由多个单条断裂组成, 断层走向为N45~60°E。

关 键 词:土壤气  汞地球化学  活断层  地震  
文章编号:1000-3274(2004)01-0132-05
修稿时间:2003年8月15日

Geochemical feature of mercury across Sanhe-Pinggu active fault
WANG Chuan-yuan,DU Jian-guo,ZHOU Xiao-cheng.Geochemical feature of mercury across Sanhe-Pinggu active fault[J].Earthquake,2004,24(1):132-136.
Authors:WANG Chuan-yuan  DU Jian-guo  ZHOU Xiao-cheng
Institution:Center for Analysis and Prediction, CSB, Beijing 100036, China
Abstract:The geochemical feature of mercy in soil-gas across the Sanhe-Pinggu active fault that was formed by strong earthquake (M8.0) in 1679 in Hebei Province, North China was discussed. Concentrations of mercury in soil gas were measured with QM201G Mercury Meter in the field. Mercury concentrations are in a wider range of 0.001~0.246 ng/L, with background value of 0.015ng/L. The zone of mercury anomalies occurs along the fracture zone and mercury density becomes as higher as 10 times compared with background value. The anomaly zones of mercury in soil gas indicate that there are two buried faults with strike of 45~60°NE, which is consistent with the reported results of geological and geophysical survey.
Keywords:Soil gas  Mercury geochemistry  Active fault  Earthquake
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《地震》浏览原始摘要信息
点击此处可从《地震》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号