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  

QUALITY AND UTILIZATION OF THE COAL FROM TAIYUAN FORMATION AND SHANXI FORMATION IN SUHAITU-KUCAOWA AREA,INNER MONGOLIA

作　　者：郭根万[1] 杨才[1] 弓贵斌[1] 

机构地区：[1]内蒙古自治区地质调查院,内蒙古呼和浩特010020

出　　处：《地质与资源》2017年第1期34-37,共4页Geology and Resources

基　　金：内蒙古自治区地质勘查基金项目"内蒙古自治区鄂托克前旗苏亥图煤炭普查"(07-1-MT01);"内蒙古自治区鄂托克前旗苦草洼北区煤炭详查"(12-1-MT03)和"内蒙古自治区鄂托克前旗苏亥图煤炭详查"(08-2-MT05)

摘　　要：苏亥图-苦草洼地区位于鄂尔多斯盆地的西部,古生界煤层的煤质为中灰、中高挥发分、中硫、低磷、低氯煤,煤类以气煤为主,局部以1/3焦煤或弱黏煤为主,可以作为炼焦配煤、动力燃料及民用煤,也可作煤的深加工原料煤等.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, mediun 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.

关 键 词：鄂尔多斯盆地 苏亥图-苦草洼地区 炼焦配煤 内蒙古 

分 类 号：P618.11[天文地球—矿床学]