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川东高陡构造成因地质模式与含气性分析
引用本文:李忠权,冉隆辉,陈更生,路中侃,段新国.川东高陡构造成因地质模式与含气性分析[J].成都理工大学学报(自然科学版),2002,29(6):605-609.
作者姓名:李忠权  冉隆辉  陈更生  路中侃  段新国
作者单位:1. 成都理工大学"油气藏地质及开发工程"国家重点实验室,成都,610059
2. 西南油气田分公司
摘    要:川东高陡构造位于四川盆地东部 ,由一系列 NE-NNE向的隔档式褶皱组成。其构造变形经历了由隔槽式褶皱到“两背一断”,最终形成隔挡式褶皱的演化过程。在“两背一断”先存构造研究基础上 ,按继承发展的观点 ,综合运用伸展构造、反转构造、断层相关褶皱等构造新理论 ,系统探讨了川东高陡构造形成演化的成因地质模式 ,结合志留系主力生烃层的生气高峰期 ,对地腹不同成因类型的构造圈闭含气性进行了分析。

关 键 词:川东  隔槽式褶皱  隔挡式褶皱  反转构造  断层相关褶皱
文章编号:1005-9539(2002)06-0605-05
修稿时间:2001年11月19日

GENETIC GEOLOGIC MODEL AND GAS-BEARING ANALYSIS OF HIGH AND STEEP STRUCTURES IN EAST SICHUAN
LI Zhong quan ,RAN Long hui ,CHEN Geng sheng ,LU Zhong kai ,DUAN Xin guo.GENETIC GEOLOGIC MODEL AND GAS-BEARING ANALYSIS OF HIGH AND STEEP STRUCTURES IN EAST SICHUAN[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2002,29(6):605-609.
Authors:LI Zhong quan  RAN Long hui  CHEN Geng sheng  LU Zhong kai  DUAN Xin guo
Institution:LI Zhong quan 1,RAN Long hui 2,CHEN Geng sheng 2,LU Zhong kai 2,DUAN Xin guo 1
Abstract:The high and steep structures in east Sichuan, located in east Sichuan Basin, are composed of ejective folds. The structural deformation has experienced the evolution from trough like folds to "two anticlines with one fault", and finally formed ejective folds. Based on the studies of pre existing structures of "two anticlines with one fault", according to the viewpoint of inheritance and development, comprehensively using the new structural theories, such as extensional structures, inversion structures, fault related folds etc., the authors systematically studied the genetic geologic model of high and steep structures and analyzed the gas bearing character of different types of subsurface structural trap by combining with the gas generating peak of the Silurian key source bed.
Keywords:east Sichuan  trough  like fold  ejective fold  inversion structure  fault related fold
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