鄂尔多斯盆地富县地区延长组长6储层特征  

CHARACTERISTICS OF THE CHANG 6 RESERVOIR OF THE FUXIAN AREA IN THE ORDOS BASIN

作　　者：张惠[1,2] 孟祥振[3] 郭艳琴[2] 张晓泉[3] 杨华[3] 刘艳[3] 冯辉[3] 

机构地区：[1]西北大学地质学系,西安710069 [2]西安石油大学油气资源学院,西安710065 [3]延长油田股份有限公司,陕西延安717111

出　　处：《石油实验地质》2010年第3期242-246,共5页Petroleum Geology & Experiment

基　　金：国家科技重大专项专题(2008ZX05005-004-08HZ);国家自然科学基金项目(40902042)联合资助

摘　　要：鄂尔多斯盆地富县地区长6油层组主要发育三角洲沉积,其中分流河道和水下分流河道是主要的油气储集层。长6油层组储集层岩石类型以岩屑长石细砂岩和长石细砂岩为主,颗粒间多为线、点—线接触,孔隙和薄膜式胶结,总体具有成分成熟度低、结构成熟度高的特征。粒间孔和长石溶孔是主要的储集空间,其中以小孔和微孔为主,渗透率小于3×10-3μm2,为特低渗储层和接近致密储层。研究区较强的压实作用、胶结作用是形成低孔低渗的主要因素,而溶蚀作用是储层物性改善的主要因素。Delta sediments are the main deposits in the Chang 6 oil beds of Yanchang Formation in Fuxian area of the Ordos Basin and the sand bodies of distributary channel and subaquatic distributary channels are main reservoirs for the hydrocarbon. Fine lithic arkose sandstone and fine arkose sandstone are main sandstones of the Chang 6 reservoir. They have line and point-line contact forms with pore and thin film cementation between rock grains. The Chang 6 reservoir is characterized by the low component maturity and high textural maturity. The main pore types are granular pore and secondary feldspar-dissolution pore which are mainly composed of small hole and micropore. The Chang 6 reservoir has super low permeability and is accessed densify reservoir of which the permeability is less than 3 × 10.3 μm2. The strong compaction and cementation are the main factors which cause the low porosity and low permeability of the reservoir, while dissolution is the main factor for improving the physical property of the reservoir.

关 键 词：成岩作用 储层特征 延长组 富县地区 鄂尔多斯盆地 

分 类 号：TE122.23[石油与天然气工程—油气勘探]