摘要
本文首先从物探、遥感和地质等方面论证了慈利—保靖深大断裂的存在,进而,根据岩性、岩相、古生物组合特征和厚度变化等阐述了该断裂的演化及煤化沥青产出的地质意义。
This paper demonstrates the presence of Cili-Baojing deep large faulting zone by a study geophysical,remote sensing and geological data.Then,the evolution of this faulting zone and the geological significance of the occurence of the carbonaceous asphaltenes are discussed on the basis of the characteris- tics of lithology sedimentary phases,and the assembly of paleontology as well as the variation of the thickness of formations.
出处
《石油勘探与开发》
SCIE
EI
CAS
CSCD
北大核心
1991年第1期7-13,共7页
Petroleum Exploration and Development
