2020
DOI: 10.1016/j.marpetgeo.2019.104152
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Characteristics of natural fractures in the upper Paleozoic coal bearing strata in the southern Qinshui Basin, China: Implications for coalbed methane (CBM) development

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Cited by 26 publications
(18 citation statements)
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“…Fracture-filling calcite belongs to epigenetic minerals arising from precipitations of hydrothermal fluids or groundwater. ,, The direction of fluid migration is controlled by fracture, so that calcite is mainly deposited and filled in a coal fracture system. The observation results using a microscope or a scanning electron microscope confirmed that the fracture can be completely or partially filled with calcite. In reality, fracture-filling calcite was commonly found in Chineselow-permeability coal seams with a high methane content, such as Carboniferous-Permian coal seam in northern China (especially in Qinshui Basin), , Late Permian coals in southwestern China (such as the coal mines in Furong, Junlian, Shiping, Huayingshan, Nantong, Liulong, and Xintian), and low-rank coals in the Fuxin basin , and southern margin of Junggar Basin . Compared with the oxidation stimulation, coal seam-acidizing treatment may have more advantages, which include: (1) acid-soluble minerals infilled in fractures are beneficial to achieve larger stimulated reservoir volumes than that by coal matrix dissolution; (2) the rate of acid–mineral reactions is much faster than that of the coal matrix oxidation reaction; and (3) acid stimulation methods have been widely used in conventional oil and gas reservoirs, and risks associated with coal acidizing can be minimized.…”
Section: Introductionmentioning
confidence: 80%
“…Fracture-filling calcite belongs to epigenetic minerals arising from precipitations of hydrothermal fluids or groundwater. ,, The direction of fluid migration is controlled by fracture, so that calcite is mainly deposited and filled in a coal fracture system. The observation results using a microscope or a scanning electron microscope confirmed that the fracture can be completely or partially filled with calcite. In reality, fracture-filling calcite was commonly found in Chineselow-permeability coal seams with a high methane content, such as Carboniferous-Permian coal seam in northern China (especially in Qinshui Basin), , Late Permian coals in southwestern China (such as the coal mines in Furong, Junlian, Shiping, Huayingshan, Nantong, Liulong, and Xintian), and low-rank coals in the Fuxin basin , and southern margin of Junggar Basin . Compared with the oxidation stimulation, coal seam-acidizing treatment may have more advantages, which include: (1) acid-soluble minerals infilled in fractures are beneficial to achieve larger stimulated reservoir volumes than that by coal matrix dissolution; (2) the rate of acid–mineral reactions is much faster than that of the coal matrix oxidation reaction; and (3) acid stimulation methods have been widely used in conventional oil and gas reservoirs, and risks associated with coal acidizing can be minimized.…”
Section: Introductionmentioning
confidence: 80%
“…Meso-and small-scale fracture parameters, including strike, dip, density, aperture, and length, are obtained through outcrops, cores, and imaging logs (Hennings et al, 2000;Khoshbakht et al, 2012). The density of meso-and small-scale fractures refers to linear density, which is the number of fractures per unit length in the normal direction of the fracture surface (Shi et al, 2020). Micro-scale fracture parameters such as length, aperture, and density are derived from thin section observation (Ameen and Hailwood, 2008).…”
Section: Data Set and Methodologymentioning
confidence: 99%
“…(a) Geographical location of the three CBM exploitation models in China. [Reproduced from ref . Copyright 2020, Elsevier.]…”
Section: Cbm Exploitation Statusmentioning
confidence: 99%