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Unconventional Natural Gas Accumulations in Stacked Deposits:A Discussion of Upper Paleozoic Coal-Bearing Strata in the East Margin of the Ordos Basin, China
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  • 英文篇名:Unconventional Natural Gas Accumulations in Stacked Deposits:A Discussion of Upper Paleozoic Coal-Bearing Strata in the East Margin of the Ordos Basin, China
  • 作者:LI ; Yong ; YANG ; Jianghao ; PAN ; Zhejun ; MENG ; Shangzhi ; WANG ; Kai ; NIU ; Xinlei
  • 英文作者:LI Yong;YANG Jianghao;PAN Zhejun;MENG Shangzhi;WANG Kai;NIU Xinlei;College of Geoscience and Surveying Engineering, China University of Mining and Technology;Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science and Technology;CSIRO Energy, Private Bag 10;China United Coal Bed Methane Co.Ltd;School of Earth and Space Sciences, Peking University;
  • 英文关键词:coal measure gas;;transitional shale gas;;tight sand gas;;three gases;;eastern Ordos Basin
  • 中文刊名:Acta Geologica Sinica(English Edition)
  • 英文刊名:地质学报(英文版)
  • 机构:College of Geoscience and Surveying Engineering, China University of Mining and Technology;Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science and Technology;CSIRO Energy, Private Bag 10;China United Coal Bed Methane Co.Ltd;School of Earth and Space Sciences, Peking University;
  • 出版日期:2019-02-15
  • 出版单位:Acta Geologica Sinica(English Edition)
  • 年:2019
  • 期:01
  • 基金:supported by the Natural Science Foundation of China(grant No.41702171);; the Beijing Municipal Excellent Talents Foundation(grant No.2017000020124G107);; 2017 Open Project Fund of State Key Laboratory of Coal Resources and Safe Mining(grant No.SKLCRSM17KFA12);; the Joint Research Fund for Overseas Chinese Scholars and Scholars in HongKong and Macao(grant No.41728005)
  • 语种:英文;
  • 页:115-133
  • 页数:19
  • CN:11-2001/P
  • ISSN:1000-9515
  • 分类号:P618.13
摘要
The Upper Paleozoic(Carboniferous to Permian) succession in the east margin of the Ordos Basin in the North China Craton has a potential to contain significant hydrocarbon resources, though attention have been mainly attracted for its successful development of coalbed methane(CBM). To improve the previous resource estimates and evaluate the hydrocarbon play possibilities, this study incorporated new discoveries of hydrocarbon units and their stratigraphic relation with source rocks, hydrocarbon migration and trapping configurations. Continuous hydrocarbon accumulation units were identified within the Upper Paleozoic, including the Taiyuan, Shanxi and Xiashihezi formations with great tight gas potential, and the Taiyuan and Shanxi formations also containing shale gas and CBM. Different strata combinations are identified with coal deposition and favour for continuous gas accumulations, including the tidal flat, deltaic and fluvial systems distributed in most of the study areas. Methane was not only generated from the thick coal seams in the Taiyuan and Shanxi formations, but also from shale and dark mudstones. The coal, shale and tight sandstones are proved of remarkable gas content and hydrocarbon indications, and the gas saturation of tight sandstones decreases upward. The stacked deposit combinations vary isochronally in different areas, while the coal seams were developed stably showing good gas sources. Two key stages control the hydrocarbon enrichment, the continuous subsidence from coal forming to Late Triassic and the anomalous paleo-geothermal event happened in Early Cretaceous, as indicated by the fluid inclusions evidence. Extensive areas show good hydrocarbon development potential presently, and more works should be focused on the evaluation and selection of good reservoir combinations.
        The Upper Paleozoic(Carboniferous to Permian) succession in the east margin of the Ordos Basin in the North China Craton has a potential to contain significant hydrocarbon resources, though attention have been mainly attracted for its successful development of coalbed methane(CBM). To improve the previous resource estimates and evaluate the hydrocarbon play possibilities, this study incorporated new discoveries of hydrocarbon units and their stratigraphic relation with source rocks, hydrocarbon migration and trapping configurations. Continuous hydrocarbon accumulation units were identified within the Upper Paleozoic, including the Taiyuan, Shanxi and Xiashihezi formations with great tight gas potential, and the Taiyuan and Shanxi formations also containing shale gas and CBM. Different strata combinations are identified with coal deposition and favour for continuous gas accumulations, including the tidal flat, deltaic and fluvial systems distributed in most of the study areas. Methane was not only generated from the thick coal seams in the Taiyuan and Shanxi formations, but also from shale and dark mudstones. The coal, shale and tight sandstones are proved of remarkable gas content and hydrocarbon indications, and the gas saturation of tight sandstones decreases upward. The stacked deposit combinations vary isochronally in different areas, while the coal seams were developed stably showing good gas sources. Two key stages control the hydrocarbon enrichment, the continuous subsidence from coal forming to Late Triassic and the anomalous paleo-geothermal event happened in Early Cretaceous, as indicated by the fluid inclusions evidence. Extensive areas show good hydrocarbon development potential presently, and more works should be focused on the evaluation and selection of good reservoir combinations.
引文
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