Through the data integration of the wells and seismic achievements and corresponding the lithofacies palaeogeographic background, the borders of the residual basin in Kong No. 2 Member are confirmed. With the help of the following methods:maturation coefficient of elastic minerals, stability coefficient of elastic heavy minerals and Universal Kriging, the recovery of the borders of the primary basin in Kong No. 2 Member is conducted. By means of comprehensive analyzing the recovery results and integrating the lithofacies palaeogeographic background, the basin borders are finally determined.
© 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 |