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《Geoscience》 1989-01
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THE METAMORPHIC EVOLUTION OF THE LATE PALEOZOIC COAL AND IT'S RANK PREDICTION IN NORTH CHINA

Yang Qi Pan Zhigui Weng Chehgmin Su Yuchun Wang Zhengping (China University of Geosicences)  
In North China, the late paleozoic coal was metamorphosed mainly to middle and high ranking in the central and southern belts, but only to low, ranking in the northern belt and southern margin. Such a feature is the comprehensive result of coal metamorphism through three evolutional stages. During the stable stage of the North China platform the late paleozoic coal evolved through geo-thermal metamorphism only to low ranking- except in some individual region, in the early mobile stage of the platform, part the Low rank coal had been promoted to medium end high metamorphic stages by additional telemagmatic metamorphism due to the strong magmatic intrusion of Yanshan Movement, in the late mobile stage the dextrally moving of the Zijingguan fault zone constructed the distribution frame of the late Paleozoic coal metamorphit: xonatioa in North China. Based upon the nature and intruding scale of the intrusives and other characteristics three subtypes of telemagmatic metamorphism are subdivided. Distribution of the telemagmatic metamorphosed coal is controlled by the Yan?shan intrusives which were intruded discontinuously along certain directions. The characteristics and determining indices of coal telemagmatic metamorphism are discussed with respect to their genesis. Taking the geologic analysis and the type of coal metamorphism as bases the rank distribution of late Paleozoic coal in North China is predicted. The predicting reserves of coking coal have been increased in the new assessment and is already partly proved by drilling.
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