2019
DOI: 10.1016/j.marpetgeo.2019.06.026
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Simulation of multi-period tectonic stress fields and distribution prediction of tectonic fractures in tight gas reservoirs: A case study of the Tianhuan Depression in western Ordos Basin, China

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Cited by 26 publications
(6 citation statements)
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“…As reported by Dang et al [16], the intermediate principal stress in Ordos basin was almost vertical. Most zones within Ordos basin are flat, so the shafts run perpendicular to the structural convergence plane, but it was oblique of the convergence plane within the orogen-basin transition zone [16,18,21]. Convergence was the independent reason for altering the orientation of intermediate principal stress.…”
Section: C-t Fractures and Discussionmentioning
confidence: 99%
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“…As reported by Dang et al [16], the intermediate principal stress in Ordos basin was almost vertical. Most zones within Ordos basin are flat, so the shafts run perpendicular to the structural convergence plane, but it was oblique of the convergence plane within the orogen-basin transition zone [16,18,21]. Convergence was the independent reason for altering the orientation of intermediate principal stress.…”
Section: C-t Fractures and Discussionmentioning
confidence: 99%
“…According to the obtained publications in the petroleum geology field, the terrains of these coalbearing basins are generally flat with almost no faults or folds growing within them. However, there are tectonic fractures that are distinguished from the diagenetic and natural fractures widely distributed within these coal-bearing basins, and this phenomenon is more remarkable near the orogen-basin transition zone [15][16][17][18][19][20][21]. The formation of tectonic fractures has been associated with convergence actions close to or even far away from strike-slip faults and transpressional structures [18,22].…”
Section: Introductionmentioning
confidence: 99%
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“…In addition, the primary joints and fissures provide a convenient channel for the water-rock reaction, which promotes crack propagation and coalescence [19][20][21]. Due to various geological tectonic effects, the minerals, joints, and fissures in soft rocks are distributed disorderly, complicating the evolution of crack propagation of soft rock [22]. Jiang et al [23] concluded that the water absorption swelling of soft rocks is anisotropic with the swelling deformation being more significant in the vertical bedding direction, and therefore, cracks are more likely to propagate in the parallel layered direction.…”
Section: Introductionmentioning
confidence: 99%
“…This Basin is a typical low-permeability formation with an average permeability of less than 1 mD. Except for the Chang 6 reservoir with developed horizontal bedding [25,26], the horizontal stress in most areas of the basin is greater than the vertical stress, which means that the fractures generated by hydraulic fracturing are mainly vertical fractures [27][28][29][30].…”
Section: Introductionmentioning
confidence: 99%