关于“碱质交代成矿模式”的几点看法
    点此下载全文
引用本文:.1989.Some opinions about metallogenic model of alkaline metasomatlsm[J].Mineral Deposits,8(3):90~96
Hits: 1865
Download times: 1318
Author NameAffiliation
赫英 西北大学地质系 
 
Some opinions about metallogenic model of alkaline metasomatlsm
Abstract:Taking Xihuashan in Jiangxi province as all example, the author advances his opinions on the “metallogenic model of alkaline metasomatism related to granites” put forward by professor Hu Shouxi et al. The geological observations and petrological mineralogical and geochemical studies have revealed the following facts: 1) The lower parts and roots of the ore veins and the related red-feldspathization are almost all confined to medium fine grained granite(γ52b), which is a product of albitization in closed and planar forms. The redfeldspathization alongside the ore veins occurs in open and linear forms and Was formed later than the albitized granite(γ52b). 2) Beneath the red-feldspathjzation zone i. e., towards the greater depth of the granite body, there is a white-albitization zone formed later than red-feldspathization. 3) The formation of ore veins ia the medimn-fine grained granite mainly proceeded downward, so the intense red-feldspathization at the root of the ore veins occurred latest and marked the end of the mineralization. 4) The red-feldspathized rock is usually in compalty with greisens. The Red-feldspathized rock in the greisen zone contains relatively high tungsten, whereas greisen in red-feldspathizatioIl zone only has rather weak mineralization. The red-feldspathized rock and greisen are two different parts separated contemporaneously from residual melt-fluids. 5) Tungsten is unevenly distributed in the Xihuashan granite body, and the lower and upper parts of the rock body show considerable difference I nits contents: from only 4.8 ppm at the depth to some 50 ppm (sporadically in excess of 100 ppm)in the upper part. Based on these facts, the author consider that the metallogenic model of alkalino metasomatism seems not to hold water in Xihuashan area.
View Full Text  View/Add Comment  Download reader
You are a visitor6398811  Beijing ICP for 05032737-5  Beijing 110102004559 male may be prepared
The Competent Units:中国科学技术协会 The Organizer :中国地质学会矿床地质专业委员会 中国地质科学院矿产资源研究所
Address: 北京市百万庄大街26号 Zip Code :100037 The Phone :010-68327284;010-68999546 E-mail: minerald@vip.163.com
本系统由北京勤云科技发展有限公司设计 
手机扫一扫