2021
DOI: 10.1016/j.jhydrol.2021.126634
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Formation mechanisms of paleokarst and karst collapse columns of the Middle Cambrian-Lower Ordovician carbonates in Huainan coalfield, Northern China

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Cited by 13 publications
(7 citation statements)
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“…Zhang et al (2021a, 2021b) used petrological, mineralogical, and geochemical methods to study the formation mechanism of KCCs in the Huainan coalfield, which they also divided into four stages. The first stage mainly occurred from the Middle Carboniferous to the Early Triassic.…”
Section: Resultsmentioning
confidence: 99%
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“…Zhang et al (2021a, 2021b) used petrological, mineralogical, and geochemical methods to study the formation mechanism of KCCs in the Huainan coalfield, which they also divided into four stages. The first stage mainly occurred from the Middle Carboniferous to the Early Triassic.…”
Section: Resultsmentioning
confidence: 99%
“…Like other areas in Northern China, the Huainan coalfield has experienced multiple stages of tectonic activities, such as the Caledonian movement in the Early Paleozoic and the Indosinian and Yanshanian movements in the Mesozoic (Shu et al, 2017;Xu et al, 2004;Zhang et al, 2022). This formed a large number of faults, folds, and fractures that became important channels for groundwater and hydrothermal fluid migration and promoted the development of paleokarst and KCCs in the Cambrian and Ordovician (Zhang et al, 2021a(Zhang et al, , 2021b. Gao (2018) found that the Huainan coalfield has 718 faults with a drop of greater than 20 m, including 532 normal faults and 186 reverse faults.…”
Section: Geological Settingmentioning
confidence: 99%
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“…With the improvement of research methods and technologies, the formation mechanism, water inrush characteristics, and water disaster prediction and prevention were analyzed. The controlling factors of paleokarst and KCCs in Huainan Mining Area were considered as strata lithology, limestone crack structure, corrosive fluids, and geological structures [10].…”
Section: Introductionmentioning
confidence: 99%