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东辛油田辛68断块周缘沉积相特征及演化
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作者 张瑞香 孔雪 +2 位作者 车雄伟 邴欣 卢文鹏 《中国石油大学胜利学院学报》 2019年第2期5-9,共5页
辛68断块基本位于辛镇长轴背斜与东营背斜的交接处,其周缘营14和营66块沙二段河道迁移摆动频繁,相带变化快,缺乏对整体区块的沉积微相认识,严重影响开发效果。结合岩性、电性及实验分析资料对辛68断块周缘营14-营66块沉积相进行研究。... 辛68断块基本位于辛镇长轴背斜与东营背斜的交接处,其周缘营14和营66块沙二段河道迁移摆动频繁,相带变化快,缺乏对整体区块的沉积微相认识,严重影响开发效果。结合岩性、电性及实验分析资料对辛68断块周缘营14-营66块沉积相进行研究。结果表明:①物缘主要来自南东方向,沙二段主要发育三角洲前缘和三角洲平原两种亚相;②沙二上1-5砂组砂体主要呈窄条带状分布,氧化色泥岩普遍存在,主要发育三角洲平原亚相;③沙二6砂组泥岩颜色自南东向北西方向由氧化色向过渡色转变,属于三角洲平原向三角洲前缘过渡相带,沙二下7-10砂组河道、河口坝砂体叠加切割连片分布,发育三角洲前缘亚相。④沙二段河道砂体自下而上逐渐向东侧方向迁移,且宽度逐渐变窄。 展开更多
关键词 岩石相特征 沉积微 沉积演化 辛68周缘
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五河地区紫苏麻粒岩岩石学特征初探 被引量:4
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作者 冉崇珍 涂荫玖 《安徽地质》 1993年第3期26-29,73,共5页
安徽蚌埠—五河地区的晚太古宙蚌埠群西堌堆组绿岩内发现了紫苏麻粒岩(暗色麻粒岩),其上、下发育有数十米厚的麋梭岩。这说明该区有高级变质的线状区域动力热流变质作用的麻粒岩相岩石存在。此发现对本区晚太古宙地壳形成的历史及其变... 安徽蚌埠—五河地区的晚太古宙蚌埠群西堌堆组绿岩内发现了紫苏麻粒岩(暗色麻粒岩),其上、下发育有数十米厚的麋梭岩。这说明该区有高级变质的线状区域动力热流变质作用的麻粒岩相岩石存在。此发现对本区晚太古宙地壳形成的历史及其变质演化过程的研究,提供了新的重要的参考资料,并对以往研究者认为本区属中低级变质的角闪岩相的结论进行了修正。 展开更多
关键词 太古宙、蚌埠群、麻粒岩岩石特征、安徽蚌埠、五河
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Petrophysical characteristics of shale oil reservoirs in the Yanchang Formation,Ordos Basin
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作者 Zhu Si-Xin An Li-Ming +2 位作者 Li Yong-Kang Zhang Xiao-Dong and Meng Fan-Ke 《Applied Geophysics》 SCIE CSCD 2022年第3期311-324,470,共15页
The mediate-low maturity continental shale oil reservoir in the 7th member of the Triassic Yanchang Formation is one of the main zones for shale oil exploration and development in Ordos Basin,China,but the seismic res... The mediate-low maturity continental shale oil reservoir in the 7th member of the Triassic Yanchang Formation is one of the main zones for shale oil exploration and development in Ordos Basin,China,but the seismic response mechanism of the reservoir remains unclear.Therefore,developing a new method for“sweet spot”seismic prediction combined with rock physics is necessary.To determine the petrophysical characteristics of continental shale in the 7th member of the Yanchang Formation in the study area,a series of tests,such as a systematic acoustic test on shale oil samples in the target segment,X-ray diffraction analyses,analysis of thin optical sections,and scanning electron microscopy,were conducted to summarize the patterns of seismic elastic property changes.Results show that the shale oil samples of the 7th member of the Yanchang Formation are primarily composed of lithic feldspar sandstone with feldspar dissolution and intergranular pores,widespread micron pores,and throats.Such composition indicates a positive correlation between porosity and permeability.The velocities of the samples are affected by their porosity and mineral composition.Velocity increases with the increase of the calcium content and decreases with the increase of the clay content,indicating a negative correlation with the porosity and total organic carbon(TOC)content on the condition of the same rock structure(quartz skeleton or clay skeleton).The elastic properties of the rock are horizontally isotropic(T1 medium),and the velocity is vertically anisotropic.In addition,the directional arrangement of clay controls the anisotropy of rock velocity.TOC is mainly distributed in the primary intergranular pores,and it has no contribution to the anisotropy of rock velocity.The results of this paper can provide a reference for the seismic prediction of continental shale oil reservoirs in the 7th member of the Yanchang Formation. 展开更多
关键词 Yanchang Formation petrophysical characteristics continental shale ANISOTROPY
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