雷竞技app官方版下载ios-雷竞技官方平台
doi: 10.11781/sysydz202402228
1.
中国石化 华东石油工程有限公司, 南京 211400
2.
长江大学 资源与环境学院, 武汉 430100
3.
中国地质大学(武汉) 资源学院, 武汉 430074
详细信息
中国石化 华东石油工程有限公司, 南京 211400
长江大学 资源与环境学院, 武汉 430100
中国地质大学(武汉) 资源学院, 武汉 430074
Fluid evolution of fracture veins of Paleogene Funing Formation in well HY1 in Subei Basin and implications for shale oil filling
1.
SINOPEC East China Petroleum Engineering Co., Ltd., Nanjing, Jiangsu 211400, China
2.
College of Resources and Environment, Yangtze University, Wuhan, Hubei 430100, China
3.
School of Earth Resources, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China
SINOPEC East China Petroleum Engineering Co., Ltd., Nanjing, Jiangsu 211400, China
College of Resources and Environment, Yangtze University, Wuhan, Hubei 430100, China
School of Earth Resources, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China
雷竞技官方平台:
苏北盆地雷竞技app官方版下载ios油勘探开发取得重大突破。高邮凹陷花页1井岩心观察发现，古近系阜宁组二段富有机质雷竞技app官方版下载ios中天然裂缝发育，脉体内保存了大量雷竞技app官方版下载ios油气流体活动迁移的信息。以阜二段雷竞技app官方版下载ios裂缝充填的方解石脉体为研究对象，综合运用矿物学、元素地球化学、地质年代学以及地质流体技术，聚焦雷竞技app官方版下载ios裂缝脉体的古流体来源、脉体形成时间以及流体包裹体特征开展深入研究，提出雷竞技app官方版下载ios含油层埋藏、抬升剥蚀过程中古温度条件与对应地质时间。阜二段雷竞技app官方版下载ios裂缝主要产状类型为层理缝、滑脱缝、剪切缝、收缩缝和张性缝，裂缝内主要充填一期纤维状方解石脉体，方解石脉体表现为偏还原环境热液流体的来源；始新世中期阜二段裂缝脉体捕获原生绿色荧光油包裹体、始新世晚期捕获次生蓝色荧光油包裹体和第四纪晚期捕获次生绿色荧光油包裹体，分别指示了富有机质雷竞技app官方版下载ios主要存在三期雷竞技app官方版下载ios油的充注过程。雷竞技app官方版下载ios油的充注主要在雷竞技app官方版下载ios最大埋深时期形成，三垛构造运动对于该地区雷竞技app官方版下载ios油的调整运移具有重要作用。
Abstract:
A significant breakthrough has been made in the exploration and development of shale oil in the Subei Basin. Cores from well HY1 in the Gaoyou Sag of Subei Basin indicate the presence of well-developed natural fractures within the organic-rich shale of the second member of Paleogene Funing Formation. These fractures contain compelling evidence of shale oil, gas, and fluid activities and migration. This study specifically examines the calcite veins filling the shale fractures within the second member of Funing Formation. Through the integration of methodologies from mineralogy, elemental geochemistry, geochronology, and geological fluid analysis, the originof paleo fluids, the timing of vein formation, and fluid inclusions within the shale fracture veins are investigated. This study also sheds light on paleotemperature conditions and corresponding geological timeframes during the burial, uplift, and denudation of the shale oil-bearing layers. The primary fracture types observed in the second member of Funing Formation include bedding fractures, detachment fractures, shear fractures, shrinkage fractures, and tensile fractures, predominantly filled with fibrous calcite veins indicating a source linked to hydrothermal fluids in a reducing environment. Notably, three distinct stages of shale oil injection are evident within the organic-rich shale fracture veins of the second member of Funing Formation, marked by primary green fluorescent oil inclusions from the Middle Eocene, secondary blue fluorescent oil inclusions from the Late Eocene, and secondary green fluorescent oil inclusions from the Late Quaternary period. The primary accumulation of shale oil occurred during the period of maximum burial depth, emphasizing the significant role of tectonic movements, especially the Sanduo tectonic event, in the redistribution and migration of shale oil in the region.
Key words:
shale fracture vein /
fluid inclusion /
fluid activity /
shale oil /
Funing Formation /
Paleogene /
Subei Basin
图 1 苏北盆地高邮凹陷构造单元和地层分布
Figure 1. Structural unit and stratigraphic distribution of Gaoyou Sag in Subei Basin
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图 2 苏北盆地高邮凹陷花页1井阜二段富有机质雷竞技app官方版下载ios裂缝脉体岩相学照片
a.层理缝脉体岩心；b.滑脱缝脉体岩心；c.张性缝脉体岩心；d.剪切缝脉体岩心。
Figure 2. Petrographic photos of fracture veins of organic-rich shale in second member of Funing Formation in well HY1, Gaoyou Sag, Subei Basin
图 3 苏北盆地高邮凹陷花页1井阜二段雷竞技app官方版下载ios裂缝脉体阴极发光照片
a，c.富有机质雷竞技app官方版下载ios纤维状方解石透射光照片；b，d.富有机质雷竞技app官方版下载ios纤维状方解石阴极发光照片。
Figure 3. Cathodoluminescence photos of shale fracture veins in second member of Funing Formation in well HY1, Gaoyou Sag, Subei Basin
图 4 苏北盆地高邮凹陷花页1井阜二段雷竞技app官方版下载ios裂缝脉体稀土元素配分模式
Figure 4. Rare earth element distribution pattern of shale fracture veins in second member of Funing Formation in well HY1, Gaoyou Sag, Subei Basin
图 5 苏北盆地高邮凹陷花页1井阜二段雷竞技app官方版下载ios裂缝脉体中流体包裹体岩相学照片
a.次生蓝白色油包裹体；b.次生绿色油包裹体；c.原生绿色油包裹体；d.次生蓝白色油包裹体；e.原生绿色油包裹体；f次生蓝白色油包裹体。
Figure 5. Petrographic photos of fluid inclusions in shale fracture veins in second member of Funing Formation in well HY1, Gaoyou Sag, Subei Basin
图 6 苏北盆地高邮凹陷花页1井阜二段雷竞技app官方版下载ios裂缝脉体中流体包裹体荧光光谱
Figure 6. Fluorescence spectra of fluid inclusions in shale fracture veins in second member of Funing Formation in well HY1, Gaoyou Sag, Subei Basin
图 7 苏北盆地高邮凹陷花页1井阜二段裂缝脉体内流体包裹体均一温度分布
Figure 7. Homogeneous temperature distribution histogram of fluid inclusions in fracture veins in second member of Funing Formation in well HY1, Gaoyou Sag, Subei Basin
图 8 苏北盆地高邮凹陷花页1井层理缝方解石脉体U-Pb同位素定年等时线
Figure 8. U-Pb isotope dating isochrones of calcite veins in bedding fractures in well HY1, Gaoyou Sag, Subei Basin
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