2019
DOI: 10.1007/s12517-019-4665-9
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Investigation of coal pore and fracture distributions and their contributions to coal reservoir permeability in the Changzhi block, middle-southern Qinshui Basin, North China

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Cited by 15 publications
(13 citation statements)
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“…76 The Changzhi block (Figure 24b), as a successive block for CBM development nowadays, is in a transition area between the east margin of Qinshui Basin synclinorium and the west edge of Taihangshan anticlinorium. 79 It belongs to a west-dipping monocline, whose orientation is NNE-NEE with an about 4°dip angle. Due to tectonic movements, major transtensional faults that are oriented at NE and NNE and minor crumples that consist of gentle folds with the orientation of NE and closed folds with the orientation of NNE and NNW develop widely in the southeast Changzhi block.…”
Section: Discussionmentioning
confidence: 99%
“…76 The Changzhi block (Figure 24b), as a successive block for CBM development nowadays, is in a transition area between the east margin of Qinshui Basin synclinorium and the west edge of Taihangshan anticlinorium. 79 It belongs to a west-dipping monocline, whose orientation is NNE-NEE with an about 4°dip angle. Due to tectonic movements, major transtensional faults that are oriented at NE and NNE and minor crumples that consist of gentle folds with the orientation of NE and closed folds with the orientation of NNE and NNW develop widely in the southeast Changzhi block.…”
Section: Discussionmentioning
confidence: 99%
“…The pores are the main location for gas accumulation, whereas coal-rock fractures are the main channels for gas flow. 13 (2) When drilling hole drainage is implemented in the working face, the drilled hole is relatively shallow and located in the pressure relief zone of coal seam. 14 16 (3) The failure of borehole seal leads to low extraction efficiency.…”
Section: Introductionmentioning
confidence: 99%
“…The Qinshui Basin of China is presently a fast-growing target block for CBM exploration and exploitation of high-rank coal in the world (Du et al, 2019; Ye et al, 2007; Zhou et al, 2016). After experiencing four-stage tectonic movements, the Qinshui Basin deformed into a synclinorium structure (Figure 1).…”
Section: Methodsmentioning
confidence: 99%