南华北中南部中新生代盆地演化与油气成藏分析  

THE MESO-CENOZOIC BASINAL EVOLUTION AND HYDROCARBON ACCUMULATION IN THE MIDDLE AND SOUTHERN PART OF SOUTHERN NORTH CHINA

作　　者：徐宏节[1] 黄泽光[2] 

机构地区：[1]成都理工大学能源学院 [2]中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所,江苏无锡214151

出　　处：《石油实验地质》2007年第6期541-544,共4页Petroleum Geology & Experiment

基　　金：中国石化科技项目(P02071)

摘　　要：南华北中南部中新生代盆地的形成演化主要受郯庐断裂带、大别造山带构造运动的制约。通过大别造山带、郯庐断裂带对南华北陆块的作用研究,以及盆地原型序列图件的编制,认为该区中新生代盆地演化经历了挤压、张扭、伸展、弱挤压等多期盆地原型的并列叠加,对油气成藏的控制起着十分重要的作用。The formation and evolution of the Meso-Cenozoic basins in the middle and southern part of southern North China was mainly controlled by the Tanlu fault system and the Dabie orogenic belt.Based on study of influence of above memtioned tectonic units on southern North China block,and what with mapping of basin prototypes,it was indicated that the Meso-Cenozoic basins underwent multiple juxtaposition and superimposition of basin prototypes with compression,tenso-shear,expanding and weak compression.All of these played a very important parts in hydrocarbon accumulation.

关 键 词：中新生代 盆地原型 油气成藏 南华北中南部 

分 类 号：TE122.3[石油与天然气工程—油气勘探]