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QUALITY AND UTILIZATION OF THE COAL FROM TAIYUAN FORMATION AND SHANXI FORMATION IN SUHAITU-KUCAOWA AREA, INNER MONGOLIA |
GUO Gen-wan, YANG Cai, GONG Gui-bin |
Inner Mongolian Institute of Geological Survey, Hohhot, China |
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Abstract The Suhaitu-Kucaowa area is located in the west of Ordos Basin, where the coal from the Paleozoic formations is characterized by medium ash content, medium-high volatile component, medium sulfur, low phosphorus and low chlorine. The coal is dominated by gas coal, with locally 1/3 coking coal or weakly caking coal, which can be used as coking blend, power fuel and domestic coal, moreover, as raw material for deep processing.
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Received: 25 April 2016
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