用户名: 密码: 验证码:
Correlation of Oil Seepages and Oil Sources and the Thrusting Nappe Structure in the South margin of the Middle Yangtze Region
详细信息   
摘要
The Jiangnan-Xuefengshan mole track is a southeast to northwest and south to north basement detachable nappe.  It formed during the Indosinian movement at the end of the Middle Triassic and compelled the Middle Paleozoic basin in south margin of the middle Yangtze region to produce a strong to weak deformation. In the front edge of the Xuefengshan nappe, a series of fault propagation anticline oil seepages developed from the Middle Paleozoic basin in the south margin of middle Yangtze region such as Cili Miaoshi, Chibi Beimencha, Jingshan Yanmenkou, and so on. The oil-source correlation indicates that these reservoirs accepted the mixed matters composed of surrounding rocks and hydrocarbon source rocks. This implicates that there may exist hydrocarbon source regions under the footwall of the thrust fault.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700