China Petroleum Exploration ›› 2024, Vol. 29 ›› Issue (2): 70-82.DOI: 10.3969/j.issn.1672-7703.2024.02.006

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Lithofacies characteristics and favorable source rock-reservoir combination of Yingxiongling shale in Qaidam Basin

Xing Haoting1,2,3, Kuang Lichun1,4, Wu Kunyu2,3, Zhang Jing2,3, Zhang Na2,3, Zhang Menglin2,3, Deng Liben2,3, Lu Zhenhua2,3, Li Yafeng2,3, Zhang Qinghui2,3   

  1. 1 College of Geosciences, China University of Petroleum (Beijing); 2 Qinghai Key Laboratory of Plateau Saline Lake Basin Oil and Gas Geology; 3 Research Institute of Exploration & Development, PetroChina Qinghai Oilfield Company; 4 Chinese Petroleum Society
  • Online:2024-03-15 Published:2024-03-15

Abstract: Yingxiongling shale in Qaidam Basin has favorable conditions for oil accumulation and enrichment, with oil resources of up to 44.5×108 t. However, the shale has a vertical thickness of more than 1000 m and the shale lithofacies and lithofacies combinations vary greatly, which bring huge challenges to the effective exploration and development of shale oil. The core sections with a length of 578 m from 12 typical wells, including Chai 2-4, Chai 906, and Chai 12 are used to analyze the petrology, organic geochemistry, and reservoir characteristics of Yingxiongling shale. The results indicate that Yingxiongling shale shows distinct characteristics of mixed sediments, with the main mineral composition of calcite, dolomite, and clay minerals, and the sedimentary structure is dominated by laminae with a size of less than 1 cm. Based on the “binary” nomenclature, five types of shale lithofacies are subdivided in the study area, namely, laminated limy dolomite, laminated dolomitic limestone, layered limy dolostone, layered dolomitic limestone, and laminated argillaceous shale. The comprehensive evaluation results of organic geochemistry and reservoir performance of various types of lithofacies show that the laminated dolomitic limestone and the layered limy dolostone are the optimum lithofacies of source rock and reservoir, respectively, with the main reservoir space of dolomite intercrystal pores. The sweet spot comprehensive evaluation results and production performance have confirmed that the interbed of layered limy dolomite and laminated dolomitic limestone is the most favorable source rock-reservoir combination pattern, showing good connectivity among sweet spots in lateral and high heterogeneity in vertical.

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