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扬子地块中、新生代构造演化对海相油气成藏的制约

郭旭升  梅廉夫  汤济广  沈传波 

摘 要:扬子地块中、新生代宏观构造演化和动力学的差异制约着中、古生界海相油气成藏.通过对扬子地块印支期以来构造演化的分析和扬子地块不同段典型油气藏的解析,显示差异的构造演化造成扬子地块不同段的主要烃流体源、保存环境和成藏演化的不同.上扬子地块的烃流体源以油裂解气和干酪根裂解气为主,海相地层中整体封闭环境发育,存在古油藏-早期气藏-晚期气藏的成藏演化系列,具有早期成藏、后期转化、晚期聚气的成藏模式.中、下扬子地块的烃流体源主要为二次生烃和海相早期原生油气源,在陆相地层与海相地层中均存在封闭体系,具有反复的成藏、改造、成藏、破坏的成藏演化过程,在断陷反转区具有下生上储、原生残余油气藏以及二次生烃等成藏模式,而在反转断块区可能的成藏模式包括原生残余成藏和晚期次生成藏.
关键词:构造演化;海相油气成藏;成藏模式;中、新生代;扬子地块
分类号:TE111.1  文献标识码:A

文章编号:0253-9985(2006)03-0295-10

Constraint of Meso-Cenozoic tectonic evolution of Yangtze massif on formation of marine reservoirs

Guo Xusheng   Mei Lianfu  Tang Jiguang  Shen Chuanbo 

 

基金项目:国家重点基础研究发展规划(973)项目(2005CB422106)
作者简介:郭旭升(1965-),男,高级工程师、博士,石油地质勘探
作者单位:郭旭升(中国石油化工股份有限公司,南方勘探开发分公司,云南,昆明,650200) 
     梅廉夫(中国地质大学,湖北,武汉,430074;中国地质大学湖北省油气勘探开发理论与技术重点实验室,湖北,武汉,430074) 
     汤济广(中国地质大学,湖北,武汉,430074) 
     沈传波(中国地质大学,湖北,武汉,430074) 

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