Abstract：The typical three-layer structural layer has been developed in the west of Tabei uplift: Cambrian-Ordovician buried hill in Paleozoic structural layer; drape anticline in Mesozoic structural layer, minor-scale of normal fault caused by differential compaction made it to be faulted anticline; the slip fold and thrust are characteristics of Cenozoic structural layer above the E1-2km gypsolith layer. The paper considered that the exploration in Mesozoic of the region should give up the mode of structural exploration and make effort to carry out lithologic exploration and exploration of small-scaled drape structure and faulted anticline.It should correctly identify a great amount of false structural images resulted from the influence of overlain gypsolith layer on seismic sections and find out reliable stratigraphic traps in combination with the study of Mesozoic sedimentary facies and microfacies and analysis of regional structural stress field and deformation feature.
罗春树, 杨金华, 李江海, 蔡振忠, 张耀堂. 塔里木盆地塔北隆起西段中生界圈闭新认识与勘探思路[J]. 石油地球物理勘探, 2007, 42(2): 226-229,234.
Luo Chun-shu, Yang Jin-hua, Li Jiang-hai, Cai Zhen-zhong, Zhang Yao-tang. New knowledge and exploration thought about Mesozoic traps in west of Tabei uplift, Tarim basin. OGP, 2007, 42(2): 226-229,234.
