Earth Science Frontiers ›› 2009, Vol. 16 ›› Issue (1): 158-166.
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College of Earth Science, Graduate University of Chinese Academy of Sciences, Beijing 100049, China
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Abstract:
Abstract: Coal is an organic rock which is sensitive to geological environmental factors such as temperature and pressure. Various tectonothermal events of the geological evolution must have caused a series of changes in physical, chemical structures of coal and thus formed different tectonically deformed coals. The effect of tectonic stress would induce the brittle and ductile deformation of coal, as well as its dynamic metamorphism at different degrees. Therefore the research about tectonic deformation and dynamic metamorphism of coal is not only of important scientific significance but also very important for the evaluation in resources of coalbed methane and the prediction of dangerous coal and gas outbursts. Based on the existing research results, different tectonic deformation and dynamic metamorphism in coal have been intensively studied through the Ro,max,XRD and NMR(CP/MAS+TOSS). Also the mechanism of dynamic metamorphism about coal under tectonic stress has been discussed. The results show that,under the influence of tectonic stress to the brittle deformation of coal, the rapid mechanical friction on the plane of fracture in the brittle deformation of coal can be translated into heat energy causing the changes of its chemical structure and composition of coal; while as to the ductile deformation coal,the accumulation of local regional strain energy can result in the failure of its chemical structure. Thus the dynamic metamorphism of different deformational mechanisms would have taken place.
Key words: Key words: coal; tectonic deformation; tectonically deformed coal; dynamic metamorphism;mechanism
Key words: coal; tectonic deformation; tectonically deformed coal; dynamic metamorphism;mechanism
CLC Number:
P618.11
P588.33
JU Yi-Wen LIN Gong LI Xiao-Shi FAN Dun-Jia. Tectonic deformation and dynamic metamorphism of coal[J]. Earth Science Frontiers, 2009, 16(1): 158-166.
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https://www.earthsciencefrontiers.net.cn/EN/Y2009/V16/I1/158