2023
DOI: 10.1016/s1876-3804(23)60417-3
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Theory, technology and practice of shale gas three-dimensional development: A case study of Fuling shale gas field in Sichuan Basin, SW China

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Cited by 10 publications
(3 citation statements)
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“…Fuling block is located in the Sichuan basin east Sichuan fold belt, the southern part of Wanxian compound dyke and the western part of Fangdoushan dorsal belt of the convergence zone Jiaoshiba tectonics, Jiaoshiba tectonics is a broken backslope, surrounded by fracture confinement, the main body of the tectonics is gentle, the depth of burial in the northeast is high, the southwest is low, and the depth of burial at the bottom of the Wufeng Formation ranges from 2250 to 5200 m. 19 The Jiaoshiba tectonics is a rhombic backslope controlled by two sets of northeastern and near-south-south oriented fractures, with an axial direction of northeast, the main body of the deformation is relatively weak, showing a box-like backslope morphology, i.e., the top of the wide and gentle stratigraphic dip is small and faults are undeveloped, while the two flanks are steeply dipping and faults are developed (Figure 1). In this study, the main target layer is the Longmaxi Formation, in which there are tectonic and diagenetic fractures in the overlying and underlying strata, and the tendency of tectonic fractures varies greatly, but the dip angle is relatively concentrated and small, and it is mainly dominated by smooth slip joints.…”
Section: Background Of the Studymentioning
confidence: 99%
“…Fuling block is located in the Sichuan basin east Sichuan fold belt, the southern part of Wanxian compound dyke and the western part of Fangdoushan dorsal belt of the convergence zone Jiaoshiba tectonics, Jiaoshiba tectonics is a broken backslope, surrounded by fracture confinement, the main body of the tectonics is gentle, the depth of burial in the northeast is high, the southwest is low, and the depth of burial at the bottom of the Wufeng Formation ranges from 2250 to 5200 m. 19 The Jiaoshiba tectonics is a rhombic backslope controlled by two sets of northeastern and near-south-south oriented fractures, with an axial direction of northeast, the main body of the deformation is relatively weak, showing a box-like backslope morphology, i.e., the top of the wide and gentle stratigraphic dip is small and faults are undeveloped, while the two flanks are steeply dipping and faults are developed (Figure 1). In this study, the main target layer is the Longmaxi Formation, in which there are tectonic and diagenetic fractures in the overlying and underlying strata, and the tendency of tectonic fractures varies greatly, but the dip angle is relatively concentrated and small, and it is mainly dominated by smooth slip joints.…”
Section: Background Of the Studymentioning
confidence: 99%
“…Coal-bed methane, shale gas, and tight sandstone gas are abundant in coal measure formations and have been of considerable interest to the energy industry in recent years. , Effective joint exploitation of coal measure gas resources is of great significance for promoting energy revolution and low-carbon green development . At present, many field tests have been carried out to develop gas exploitation through single reservoirs by using fracturing techniques. However, the joint exploitation of the gas through multi-reservoirs through fracturing techniques is still in its early stages.…”
Section: Introductionmentioning
confidence: 99%
“…Important discoveries were made successively in some organic-rich continental shale formations. These included the Permian Lucaogou Formation in the Jimusar Sag of the Junggar Basin [3][4][5][6], the 7 3 Sub-member of the Triassic Yanchang Formation in the Ordos Basin [7,8], the Second Member of the Paleogene Kongdian Formation in the Cangdong Sag at the center of the Bohai Bay Basin [9,10], the Third and Fourth Members of the Paleogene Shahejie Formation in the Boxing Sag, the Niuzhuang Sag, and the Bonan Sag of the Jiyang Depression [11][12][13], the First and Second Members of the Cretaceous Qingshankou Formation in the Songliao Basin [14][15][16][17][18], and the Jurassic shales in the northeastern Sichuan Basin [19,20]. These shale formations show bright prospects for the development of continental shale oil.…”
Section: Introductionmentioning
confidence: 99%