塔北与塔中地区奥陶系碳酸盐岩储层成因对比研究  

Comparative study of the genesis of the Ordovician carbonate reservoir rocks in northern and central Tarim Basin,Xinjiang

作　　者：阮壮[1] 于炳松[2] 李朝晖[3] 谭广辉[1] 

机构地区：[1]中国石油大学油气资源与探测国家重点实验室,北京102249 [2]中国地质大学地质过程与矿产资源国家重点实验室,北京100083 [3]吉林油田勘探开发研究院,吉林松原138000

出　　处：《沉积与特提斯地质》2010年第3期84-89,共6页Sedimentary Geology and Tethyan Geology

基　　金：国家自然科学基金项目(40472064;40672079);中国地质大学(北京)海相储层演化与油气富集机理教育部重点实验室开放基金项目(2008-01)

摘　　要：通过储层发育层段、储层类型、沉积演化、岩溶作用等方面的对比,发现塔北与塔中地区奥陶系碳酸盐岩储层在发育层位、沉积演化及岩溶期次上既有相似性,也有差异性。在塔中地区的油气勘探中,应注意下奥陶统古风化壳岩溶发育与塔北地区的差异性,加强对上奥陶统礁滩储集体的勘探。The comparative study of reservoir horizons,reservoir types,sedimentary evolution and karstification phases indicates that there are both similarities and differences in reservoir horizons,sedimentary evolution and karstification phases of the Ordovician carbonate reservoir rocks in northern and central Tarim Basin,Xinjiang.In the petroleum exploration in central Tarim Basin,particular attention should be drawn to the Upper Ordovician reef reservoirs due to their differences in the development of palaeo-weathering crust karsts in the Lower Ordovician strata in northern Tarim Basin.

关 键 词：塔里木盆地 奥陶系 碳酸盐岩储层 岩溶作用 

分 类 号：TE122.221[石油与天然气工程—油气勘探]