Formation mechanism and geological significance of shale reservoirs in Cretaceous continental faulted basins of the Yanshan Tectonic belt, Northeastern China: A case study of the Luanping Basin

被引:0
作者
Yuan, Xiaodong [1 ]
Zhang, Yuanfu [1 ,2 ]
Jiang, Zaixing [1 ,2 ]
Liu, Xiaoning [1 ]
Huo, Yancui [1 ]
Ge, Pengcheng [1 ]
机构
[1] China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China
[2] China Univ Geosci, Inst Earth Sci, Beijing 100083, Peoples R China
关键词
Continental faulted basins; Shale reservoir; Volcanic activity; Luanping Basin; Yanshan Tectonic Belt; OIL; EXPLORATION; PETROLEUM; TEXAS;
D O I
10.1016/j.jseaes.2024.106472
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Shale oil and gas exploration in China has primarily focused on medium- to large-sized basins, with relatively few breakthroughs in small basins, particularly those within tectonic belts. The complexity of sedimentary environments in continental faulted basins often results in significant variations in shale oil and gas properties; thus, evaluating the potential in such basins is challenging. Luanping Basin is a typical faulted basin within the Yanshan Tectonic Belt. The successful drilling of Well LT1 marks the first exploration breakthrough for shale oil and gas in this region. This study analysed and evaluated the shale oil and gas characteristics in the Luanping Basin through lithofacies identification, sedimentary stage division, reservoir porosity and permeability features, sedimentary environmental analysis, and shale oil and gas properties. These results indicate that the Xiguayuan Formation in the Luanping Basin can be divided into five sedimentary stages based on volcanic activity characteristics. Stages 1-3, influenced by volcanic and hydrothermal activity, are the primary oil- and gas-producing layers. The reservoir space types include pores within the clay, dissolution, OM-hosted, intercrystalline, and intercrystal pyrite pores, grain-edge structural, and hydrocarbon generation fractures. Based on the total organic carbon (TOC) content, mineral composition, and sedimentary structure, nine lithofacies types were identified, with middle organic matter-laminated siliceous shale being the most favourable lithofacies type for shale oil and gas. The shale oil density was 0.75 g/cm3, viscosity was approximately 10 mPa & sdot;s, and the GOR ratio was as high as 980, which is superior to some developed continental basins in China. Sedimentary environmental analysis suggests that shale oil and gas developed in a semi-arid, semi-saline water sedimentary environment influenced by multiple sources, such as terrestrial, volcanic, and hydrothermal materials. This environment resulted in a higher reservoir brittleness index and significantly affected the hydrocarbon generation potential of the source rocks. Successful exploration in the Luanping Basin demonstrates that high-quality source rocks and reservoirs can form in complex tectonic belts with semi-arid lake environments, producing high-quality shale oil and gas resources, highlighting their unique characteristics.
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页数:21
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