内蒙古乌审旗板户梁方沸石岩矿特征及开发应用前景  

Features and Exploiting Future on BanhuliangAnalcite Deposit in Wushen Banner, Inner Mongolia

作　　者：刘丽萍 关爱凤 梁永 高荣宽 熊煜 

机构地区：[1]内蒙古地质矿产勘查院,内蒙古呼和浩特010010

出　　处：《内蒙古地质》2002年第1期20-26,共7页Geology of Inner Mongolia

摘　　要：内蒙古乌审旗板户梁方沸石岩矿赋存在下白垩统志丹群洛河组二段二亚段紫红色泥岩和方沸石泥岩中,矿体呈近水平层状产出,为内蒙古地区乃至国内少见的大型矿床。方沸石是沸石族矿物的一种,具有独特的理化特征,可被广泛应用于工业、农业、建筑业、化工业、废水处理等方面。Banhuliang analcite deposit is a newly discovered large deposit, which is rare in Inner Mongolia, even in China. It occurs approximately horizontal in purplish-red and analcite mudstone of the second subsection of Luohe Group's second section in Lower Cretaceous. Analcite belongs to zeolitic minerals family, and has unique physical and chemical features. It can be widely applied in many fields, such as industry, agriculture, architecture, chemical industry and wastewater procession.

关 键 词：乌审旗 方沸石 地质及理化特征 

分 类 号：P578[天文地球—矿物学]