Restoration of Paleoformation Pressure of Shale in the 3rd Member ofShahejie Formation and Its Application in Eastern Slope of Jinxian1-1 Low Uplift, Liaodong Bay Fault Depression

Abstract

Abstract:

Overpressure in shale is the main force for hydrocarbon expulsion and primary migration, and its changes are always recorded by the evolution of shales porosity. Firstly, the evolution module of shales porosity in undercompacted shale was set up through compaction section reflecting the characteristic of compaction at present. And then the method of “regressive extrapolation” modeling was used to restore evolution porosity increment of paleoporosity shale in hydrocarbon accumulation period. Based on this restoration, the total porosity of undercompacted shale could be figured out by the evolution module of shales porosity. Finally, modified Phillippone formula could be used to calculate paleoformation pressure of source rocks and to recover evolution of paleoformation pressure. The result showed that overpressure of source rock of the 3rd Member of Shahejie Formation enhanced gradually from south to north in eastern slope of Jinxian 1-1 low uplift, and the change regular of paleoformation pressure was important for hydrocarbon migration and profitable target selection.

Key words: the eastern slop of Jinxian 1-1 low uplift, the 3rd Member of Shahejie Formation, source rock, mudstone paleo porosity, shale paleo formation pressure

CHEN Kai, LIU Shen, SHU Wen-Ai, ZHOU Xin-Fu, ZHANG Rong-Hui. Restoration of Paleoformation Pressure of Shale in the 3rd Member ofShahejie Formation and Its Application in Eastern Slope of Jinxian1-1 Low Uplift, Liaodong Bay Fault Depression[J]. Geoscience, 2012, 26(3): 540-546.

References

［1］李明诚.石油与天然气运移
[M]. 第二版.北京:石油工业出版社，1994：20-70.
［2］吕延防.油气藏封盖研究
[M].北京:石油工业出版社,1996：5-105.
［3］刘震，张万选，张厚福，等.辽西凹陷北洼下第三系异常地层压力分析
[J].石油学报，1993，14(1)：14-23.
［4］Roedder E, Bodnor R J. Geological pressure determining from fluid inclusion studies
[J]. Annual Review of Earth and Planetary Sciences, 1980, 8: 263-301.
［5］陈勇,周瑶琪,倪培.一种获取包裹体内压的新方法——二氧化碳拉曼光谱法
[J]. 岩矿测试,2006,25(3):211-214.
［6］米敬奎，肖贤明，刘德汉，等.利用储层流体包裹体的PVT特征模拟计算天然气藏形成古压力：以鄂尔多斯盆地上古生界深盆气藏为例
[J].中国科学：D辑，2003，33(7)：679-685.
［7］Hottman C E, Johnson R K. Estimation of formation pressures from logderived shale properties
[J]. Joural of Petroleam Technology,1965,17(6)：717-722.
［8］付广，张发强. 利用声波时差资料研究欠压实泥岩盖层古压力封闭能力的方法
[J].石油地球物理勘探，1998,33(6):812-818.
［9］付广，吕延防，杨勉. 欠压实泥岩异常孔隙流体压力的定量研究
[J].新疆石油地质,2002,23(4):295-298.
［10］刘福宁.异常高压区的古沉积厚度和古地层压力恢复方法探讨
[J].石油与天然气地质，1994，15(2)：180-185.
［11］Magara K. Comparison of porositydepth relationships of shale and sandstone
[J]. Journal of Petroleum Geology, 1980, 3(2): 175-185.
［12］Dutta T, Mavko G, Mukerji T, et al. Compaction trends for shale and clean sandstone in shallow sediments, Gulf of Mexico
[J]. The Leading Edge, 2009, 28(5): 590-596.
［13］Nakayama. Simulation model for petroleum exploration
[J]. AAPG Bulletin,1981, 65(7): 1230-1255.
［14］王震亮,罗晓容,陈荷立.沉积盆地地下古流体动力场恢复
[J].西北大学学报：自然科学版,1997,27(2):155-159.
［15］王震亮，陈荷立. 鄂尔多斯盆地中部上古生界古流体动力分析
[J]. 沉积学报，1998，12(4)：105-108.
［16］王震亮. 准噶尔盆地古水动力模拟参数研究
[J].西北大学学报：自然科学版,2001，31(2)：153-156.
［17］刘震. 储层地震地层学
[M]. 北京: 地质出版社, 1997：30-70.
［18］李鹤永，刘震，马达德，等. 柴西地区古流体势场演化对油气藏的控制作用
[J]. 石油大学学报：自然科学版，2005,29(3)：12-16.
［19］刘震,邵新军,金博,等. 压实过程中埋深和时间对碎屑岩孔隙度演化的共同影响
[J]. 现代地质, 2007, 21(1): 125-132.
［20］邵新军,刘震,崔文富. 沉积盆地地层古埋深的恢复
[J].石油勘探与开发, 1999, 26(3):33-35.
［21］Terzaghi K. Theoretical Soil Mechanics
[M]. New York: John Wiley and Sons, 1953：75-80.
［22］Wyllie M R J, Gregory A R, Gardner L W. Elastic wave velocities in heterogeneous and porous media
[J]. Geophysics, 1956, 21(1): 41-70.
［23］Wyllie M R J, Gardner G H F, Gregory A R. Some phenomena pertinent to velocity logging
[J]. Journal of Petroleum Technology, 1961, 13(7): 629-636.

[1]	KE Xing, ZHAO Qingfang, WU Piao, YANG Chuansheng, LIAO Jing, GONG Jianming. Characteristics and Evaluation of Cretaceous Source Rocks in the Northeastern Jiaolai Basin [J]. Geoscience, 2023, 37(05): 1358-1368.
[2]	YANG Xiongbing, WANG Hongyu, SU Yushan, GUAN Chao. Source Rock Characteristics and Its Accumulation Contribution in the Lower Congo Basin, South Atlantic [J]. Geoscience, 2023, 37(05): 1369-1384.
[3]	GAN Jun, JI Hongquan, LIANG Gang, HE Xiaohu, XIONG Xiaofeng, LI Xing. Gas Accumulation Model of Mesozoic Buried Hill in Qiongdongnan Basin [J]. Geoscience, 2022, 36(05): 1242-1253.
[4]	ZHANG Yingzhao, HU Senqing, LIU Jinshui, JIANG Yiming, CHEN Zhongyun, QIN Jun, DIAO Hui, WANG Chao. Geochemical Characteristics and Genesis of Oil and Gas in the Lishuixi Sag, East China Sea Shelf Basin [J]. Geoscience, 2022, 36(05): 1382-1390.
[5]	ZHENG Qinghua, LIU Xingjun, ZHANG Xiaolong, WANG Hongjun, LIAO Yongle, AN Erliang, LIU Tao, ZHANG Jianna, ZUO Qin. Review of the High Natural Gamma Sandstones Associated With Source Rocks in the Chang 7₃ Submember of the Yanchang Formation, Ordos Basin [J]. Geoscience, 2022, 36(04): 1087-1094.
[6]	FAN Yan, WANG Xulong, XIANG Caifu, WANG Qianjun, LIU Jia, LIAO Jiande, XU Huaimin. Enrichment Patterns and Main Controlling Factors of Source Rocks in the Permian Pingdiquan Formation, Eastern Junggar Basin [J]. Geoscience, 2022, 36(04): 1105-1117.
[7]	GAO Yangdong, LIN Heming, WANG Xudong, QIU Xinwei, QUE Xiaoming, LI Min, ZHAO Zeying, CHEN Yan. Geochemical Constraints on the Sedimentary Environment of Wenchang Formation in Pearl River Mouth Basin and Its Paleoenvironmental Implications [J]. Geoscience, 2022, 36(01): 118-129.
[8]	LI Yan, DENG Yunhua, LI Youchuan. Characteristics and Mechanism of Source Rock Development Controlled by Sedimentary Microfacies in River-delta System: Case Study of Coal-measure Source Rock in Enping Formation in Pearl River Estuary Basin [J]. Geoscience, 2021, 35(04): 1065-1077.
[9]	QI Peng, GUO Gang, REN Yaping, CUI Min, WANG Xin. Geological Characterization of the Eocene Pinghu Movement in the Xihu Sag and Its Hydrocarbon Geological Significance [J]. Geoscience, 2021, 35(04): 1098-1105.
[10]	SHEN Hua, LIU Zhen, SHI Yuanpeng, XU Zeyang, LI Yongjun, CHEN Shuguang, WANG Huilai, WANG Zhicheng, WANG Biao, LIU Chang. Hydrocarbon Accumulation Process and Exploration Potential in Linhe Depression, Hetao Basin [J]. Geoscience, 2021, 35(03): 871-882.
[11]	JIANG Wei, GAO Zhiqian, HU Zongquan, ZHAO Yongqiang, CHU Chenglin. Sedimentary Filling Evolution and Hydrocarbon Control of High Frequency Sequence in Yurtus Formation, Tarim Basin [J]. Geoscience, 2021, 35(02): 349-364.
[12]	ZHAO Yande, DENG Xiuqing, QI Yalin, SHAO Xiaozhou, YANG Bin, LU Xinchuan, LUO Anxian, XIE Xiankui. Geochemical Characteristics of Source Rocks of M53 Well and Chang-8 Member Oil-source in Pingliangbei Exploration Area, Ordos Basin [J]. Geoscience, 2020, 34(04): 800-811.
[13]	ZHANG He, JIANG Zhenglong, LI Yajun, LIANG Shuang, FU Wenkai. Hydrocarbon Generation Conditions and Regional Comparison of the Lower Jurassic Kangsu Formation in Washixia Sag, Tarim Basin [J]. Geoscience, 2019, 33(06): 1241-1251.
[14]	QI Yulin, ZHANG Zhihuan, XIA Dongling, ZHANG Huimin, HUANG Caixia, ZHENG Duo, JIN Xiao, CAO Yongle, ZHU Lei. Comparative Analysis of Hydrocarbon Generation Kinetics of Dark Shale and Black Shale of Chang 7 in Southern Ordos Basin [J]. Geoscience, 2019, 33(04): 863-871.
[15]	XI Shengli, GANG Wenzhe, YANG Qingyu, CHEN Guo, LIU Yazhou, WANG Ning, LIU Lan. Organic Geochemistry and Sedimentary Paleoenvironment of Chang 7 Source Rocks in Yanchi-Dingbian Area, Ordos Basin [J]. Geoscience, 2019, 33(04): 890-901.