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.
郭根万, 杨才, 弓贵斌. 内蒙古苏亥图-苦草洼地区太原组和山西组煤质特征及综合利用研究[J]. 地质与资源, 2017, 26(1): 34-37.
GUO Gen-wan, YANG Cai, GONG Gui-bin. QUALITY AND UTILIZATION OF THE COAL FROM TAIYUAN FORMATION AND SHANXI FORMATION IN SUHAITU-KUCAOWA AREA, INNER MONGOLIA. GEOLOGY AND RESOURCES, 2017, 26(1): 34-37.
2017, Vol. 26 
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