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湘黔边境重晶石矿成矿地质背景及成矿模式浅析
引用本文:杨义录.湘黔边境重晶石矿成矿地质背景及成矿模式浅析[J].贵州大学学报(自然科学版),2010,27(1):43-48.
作者姓名:杨义录
作者单位:贵州省地质矿产勘查开发局101地质大队,贵州,凯里,556000
摘    要:重点论述贡溪-坪地向斜重晶石矿形成的地质背景,认为重晶石矿仅产出于坪地-贡溪向斜南东翼圭勺-虾麻塘-大河边-冲磨一线地幔热隆起带的东侧,提出该重晶石矿的成矿模式。该模式在江南地层区的古沉积盆地中寻找同类型成因的重晶石及其他热水沉积矿床,特别是Ni、Mo、V等多金属矿床,有重要指示意义。

关 键 词:重晶石  地质背境  成矿模式  湘黔

The Metallogenic Geological Background and Metallogenic Model of the Barite Mineral in Hunan-Guizhou Border
YANG Yi-lu.The Metallogenic Geological Background and Metallogenic Model of the Barite Mineral in Hunan-Guizhou Border[J].Journal of Guizhou University(Natural Science),2010,27(1):43-48.
Authors:YANG Yi-lu
Institution:101 Geological Group;Guizhou Bureau of Geology and Mineral Exploration & Development;Kaili 556000;China
Abstract:The geological background of the barite mineral formation in the Gongxi-Pingdi Synclinal structure was discussed.Considering the barite mineral was only produced in the east of the mantle Hot bulge,along the line from the South East Wing of Guishao in Pingdi-Gongxi Synclincal structure-Xiamatang-Dahebian-Chongmo,the Metallogenic model of the barite mineral was proposed.This model has important implications for searching the same type of causes of barite mineral or other hot-water Sedimentary deposits in the...
Keywords:barite  Geological background  metallogenic model  Xiangqian  
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