延安以南地区奥陶系碳酸盐岩储层中流体包裹体及烃类物质的油气指示意义
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伊硕(1989—),女,河北涿州人,博士,主要从事碳酸盐岩储层评价等研究工作。联系电话:18810109251,E-mail:yishuo2010@163.com。

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国家自然科学基金项目“鄂尔多斯盆地煤中稀土元素分布与赋存特征及其地质意义”(41472136),中央高校基本科研业务费专 项资金“鄂尔多斯盆地东南部马五段白云岩成因及分布规律研究”(2-9-2016-116)。


Fluid inclusions and hydrocarbons in Ordovician carbonate reservoirs in the South of Yan’an and its implication for oil and gas
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    摘要:

    为明确鄂尔多斯东南部延安以南地区奥陶系储层中流体包裹体及烃类物质的油气指示意义,对其流体包裹 体的岩相学、均一温度和盐度及组分特征进行综合分析,并结合研究区埋藏-热演化史,探讨储层烃类充注史。根 据流体包裹体室温下的相态特征、组分和烃类分布产状,可将研究区碳酸盐岩储层流体包裹体分为盐水包裹体、气 态烃包裹体、液态烃包裹体、沥青包裹体及含烃气-液两相盐水包裹体5类,局部还存在残余游离液态烃和运移沥青 等未形成流体包裹体的烃类物质。研究表明,研究区流体包裹体及烃类物质主要分布在充填于储层孔隙、溶洞、裂 缝中的方解石、石英等自生矿物内,均一温度随盐度升高逐渐递增,所捕获的流体包裹体主要为烃源岩在高成熟阶 段的产物。奥陶系碳酸盐岩储层曾在中侏罗世末期和早白垩世末期发生过2期油气充注,且以早白垩世末期为主。

    Abstract:

    To clarify the indicative significance of fluid inclusions and hydrocarbons in Ordovician carbonate reservoirs in the South of Yan’an,southeast of Ordos,a comprehensive analysis of the petrology,homogenization temperature,salinity and compositional characteristics of fluid inclusions was carried out. Combined with the burial history and thermal evolution of the study area,the hydrocarbon charging history of the reservoir was discussed. According to the phase characteristics,components and hydrocarbon occurrence distribution of fluid inclusions at room temperature,the fluid inclusions of carbonate reservoirs in the study area can be divided into five categories:aqueous inclusions,gaseous hydrocarbon inclusions,liquid hydrocarbon inclusions,bituminous inclusions,hydrocarbon-bearing aqueous two-phrase fluid inclusions,and there are still local residual free liquid hydrocarbons and migrabitumen which do not form fluid inclusions. The results show that the fluid inclusions and hydrocarbons in the study area are mainly distributed in authigenic minerals such as calcite and quartz that fill the pores,the cavities and the fractures of the reservoir. The homogenization temperature gradually increases with the increasing salinity,and the captured fluid inclusions are mainly the products of the source rocks in the high maturity stage. The Ordovician carbonate reservoirs were charged in two stages,the end of the middle Jurassic and the late of the early Cretaceous,and the latter is the main stage.

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伊硕,黄文辉,王一刚,文应初.延安以南地区奥陶系碳酸盐岩储层中流体包裹体及烃类物质的油气指示意义[J].油气地质与采收率,2018,25(6):38~44

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  • 在线发布日期: 2019-01-17