我国温石棉矿床产出构造环境及成因分类探讨  

Discussion on Structural Setting and Genetic Classification of Asbestoide Deposits in China

作　　者：许仲华 罗勇 

机构地区：[1]四川省地矿局川东南地质大队

出　　处：《建材地质》1989年第4期9-16,共8页

摘　　要：温石棉矿床成因分类,是在热液成矿作用二级分类的前提下,按照含矿围岩的建造类型、产出构造环境、成矿热液来源等条件而进行的三级分类。按建造类型,分为镁质碳酸盐岩蚀变型及镁质超基性岩蚀变型两个大类,再按大地构造位置和成矿热液的来源不同,划分为七个类型。其中镁质碳酸盐岩蚀变型有三个(Ⅰ_1—Ⅰ_3),镁质超基性岩蚀变型四个(Ⅱ_1—Ⅱ_4)。Genetic classification of asbestoide deposits is a grade-Ⅲ classification, in terms of formational types, structural setting, origin of hydrothermal etc. on the premise of hydrothermal mineralization grade-Ⅱ classification. On the basis of formational types, these deposits can be classified two types, that is, altered magnesian carbonate rock type and altered magnesian ultrahasic rock type. According to tectonic location and different origin of hydrothermal, they can be further classified seven subdivisions, in which there are three subdivisions (Ⅰ_1-Ⅰ_3) belonging to altered magnesian carbonate rock type and four subdivisions (Ⅱ_1-Ⅱ_4) belonging to altered magnesian ultrabasic rock type.

关 键 词：温石棉矿床 构造环境 成因 分类 

分 类 号：P619.271[天文地球—矿床学]