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作 者:杨杰[1]
机构地区:[1]延长油田股份有限公司永宁采油厂勘探科,陕西延安716000
出 处:《岩性油气藏》2013年第6期25-29,共5页Lithologic Reservoirs
基 金:陕西省自然科学基础研究计划项目"鄂尔多斯盆地致密砂岩油藏成藏物性下限研究"(编号:2013JM5007);陕西省教育厅专项科研计划项目"鄂尔多斯盆地延长组深层石油成藏机理研究"(编号:12JK0491)联合资助
摘 要:根据岩石薄片、铸体薄片、扫描电镜、黏土矿物X射线衍射、压汞和物性分析等资料,对延安地区长4+5油层组致密砂岩储层特征进行了研究.结果表明:延安地区长4+5油层组储层岩石类型主要为细粒长石砂岩;孔隙度和渗透率分别为6.0%~10.0%和0.2~2.0mD,为典型的致密砂岩储层;储集空间主要为残余粒间孔,其次为长石和浊沸石溶孔;孔隙结构以小孔细喉型为主,其次为小孔中细喉型和细孔微细喉型;压实作用及绿泥石、方解石和浊沸石胶结作用是造成储层物性变差的主要因素,而溶蚀作用在一定程度上改善了储层物性.该研究成果为延安地区长4+5油层组致密砂岩油藏滚动勘探开发提供了地质依据.According to the data of rock thin section, cast thin section, scanning electron microscope, X diffraction of clay minerals, high pressure mercury and properties analysis, this paper studied the characteristics of tight sandstone reservoir of Chang 4+5 oil reservoir set in Yan 'an area. The results show that the rock type of Chang 4+5 sandstone reservoir is mainly fine-grained feldspar sandstone; porosity and permeability range from 6.0% to 10.0% and 0.2 mD to 2.0 mD respectively, and the reservoir belongs to typical tight sandstone reservoir; reservoir space is mainly residual intergranular pores, followed by dissolved pores in feldspar and laumontite; pore structure is dominated by small pore and fine throat type, followed by fine throat and pore tiny throat type; compaction and cementation in chlorite, calcite and laumontite are the main factor for causing poor reservoir properties, and dissolution improves reservoir properties. The results of this study provide a geological basis for rolling exploration and development for Chang 4+5 oil reservoir set in Yan' an area.
关 键 词:致密砂岩 储层特征 成岩作用 长4+5油层组 鄂尔多斯盆地
分 类 号:TE122.23[石油与天然气工程—油气勘探]
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