全球奥陶系碳酸盐岩油气藏综述A REVIEW OF THE ORDOVICIAN CARBONATE RESERVOIRS IN THE WORLD
王建坡,沈安江,蔡习尧,罗友成,李越
摘要(Abstract)：
奥陶系碳酸盐岩油气田主要分布于北美、北欧、中国和澳大利亚。在北美,油气藏主要分布于下奥陶统El-lenburger组选择性白云岩化和经喀斯特改造的碳酸盐岩层系中;上奥陶统的Trenton-Black River灰岩,特别是Trenton灰岩段的构造破碎和白云岩化作用是影响油气成藏的主控因素;Red River组油藏则受控于构造圈闭。北欧哥特兰岛Klasen灰岩储集空间则以灰泥丘原生孔隙和断裂、缝合线为主。中国奥陶系油气藏分布于鄂尔多斯盆地和塔里木盆地,成藏条件相对复杂:在鄂尔多斯盆地,主要与膏云岩经大气淡水淋滤作用形成的风化壳密切相关,也有白云岩、生物礁等多种储集体;而塔里木盆地塔中地区储集体集中于礁滩相,还包括台地灰岩和台缘浅滩白云岩等其他相带,沉积间断面上的古喀斯特作用是成藏的主控因素。澳大利亚的坎宁盆地是较新的勘探区,其油气聚集方式与北美Ellenburger组相似。
关键词(KeyWords)： 碳酸盐岩油气储层;奥陶系;中国;北美;哥特兰岛;瑞典;澳大利亚
基金项目(Foundation): 中国科学院创新工程方向性项目(KZCX2-YW-122,KZCX3-SW-149);; 国家自然科学基金项目(No.40572069,40532009);; 国家重点基础研究发展计划项目(2006CB806402)
作者(Author): 王建坡,沈安江,蔡习尧,罗友成,李越
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