江南—雪峰隆起构造动力学与海相油气成藏演化  

Tectonic Dynamics and Marine Hydrocarbon Accumulation of Jiangnan-Xuefeng Uplift

作　　者：梅廉夫[1] 邓大飞[1] 沈传波[1] 刘昭茜[1] 

机构地区：[1]中国地质大学构造与油气资源教育部重点实验室,武汉430074

出　　处：《地质科技情报》2012年第5期85-93,共9页Geological Science and Technology Information

基　　金：国家科技重大专项"南方海相层系油气成藏与富集规律研究"(2011ZX05005-003-007)

摘　　要：研究讨论了我国南方江南-雪峰隆起这一独特的大地构造单元在板块构造阶段和大陆构造阶段的发育背景及其构造动力学。在此基础上阐述了江南-雪峰隆起及其周缘的海相油气聚集、破坏的特征和背景(构造动力学框架下),研究试图揭示隆起及其周缘的海相油气聚集和破坏与隆起形成演化及其动力学之间在时间和空间上的成因联系。最后讨论了隆起在板块构造与大陆构造不同阶段演化和动力学问题、板块构造与大陆构造观点对隆起及其周缘成藏物质基础制约的不同认识、以及隆起及其周缘构造演化与海相油气成藏演化的关系。Based on plate tectonics stage and continental dynamics stage, the study discusses the development background and tectonic dynamics of Jiangnan-Xuefeng uplift, which is the unique tectonic units of the South China. On this basis, the paper introduces the features and background about the marine hydrocarbon accumulation and destruction of Jiangnan-Xuefeng uplift and its circumference. The study attempts to reveal the relationship in time and space between the marine hydrocarbon accumulation/destruction and the dynamics evolution of Jiangnan-Xuefeng uplift and its circumference. Finally, we discuss the formation evolution and dynamics of the uplift at the different stages of plate tectonics and continental tectonics, hydrocarbon accumulation, and the relationship between tectonic evolution and hydrocarbon accumulation evolution of Jiangnan-Xuefeng uplift and its circumference.

关 键 词：构造动力学 海相地层 成藏 江南-雪峰隆起 

分 类 号：P618.130.2[天文地球—矿床学]