徐家围子断陷CO_2气藏形成地质机制研究  

GEOLOGICAL MECHANISM OF THE FORMATION OF CO_2 RESERVOIR OF XUJIAWEIZI RIFT

作　　者：迟元林[1] 云金表[1] 庞庆山[2] 

机构地区：[1]长春科技大学,吉林长春130026 [2]大庆石油学院,黑龙江安达151400

出　　处：《大庆石油地质与开发》2000年第3期1-3,共3页Petroleum Geology & Oilfield Development in Daqing

摘　　要：应用地震、地质解释与地球化学分析方法从区域构造特征、区域断裂系统与火山岩成因、区域深部地质特征、热流底辟体分析等 ,深入分析CO2 气的成因、成藏模式与过程 ,为深层CO2This paper analyzes the regional structural characteristic, regional fracturing system and volcanic rock genesis, regional deep geological characteristic and heat flow diapir body with seismic, geological interpretation and geochemical analytical methods. Then it analyzes the genesis of CO\-2, reservoir formation pattern and process so as to propose a new point of view for further exploration.

关 键 词：徐家围子断陷 气藏 深部地质 成藏 二氧化碳 

分 类 号：P618.130.1[天文地球—矿床学]