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桂西铝多金属矿床地质地球化学特征与成矿机理
引用本文:戴塔根,龙永珍,张起钻,胡斌.桂西铝多金属矿床地质地球化学特征与成矿机理[J].地球科学与环境学报,2007,29(4):345-350.
作者姓名:戴塔根  龙永珍  张起钻  胡斌
作者单位:1. 中南大学,地质研究所,湖南,长沙,410083
2. 广西地质勘查局,广西,南宁,530023
基金项目:广西新世纪十百千人才工程基金
摘    要:对桂西地区铝土矿及其围岩系统取样,进行了微量元素分析。结果表明,原生铝土矿的成矿母岩主要为下二叠统茅口灰岩,其次有少量古陆风化物的加入;区内原生铝土矿形成于海相的沉积环境,堆积型铝土矿由原生沉积型铝土矿风化淋滤而成。

关 键 词:铝多金属矿床  微量元素  地球化学  成矿机理  桂西
文章编号:1672-6561(2007)04-0345-06
修稿时间:2006年12月20

Geological and Geochemical Characteristics and Metallogenic Mechanism of Aluminium Multi-Metal Deposits in Western Guangxi
DAI Ta-gen,LONG Yong-zhen,ZHANG Qi-zuan,HU Bin.Geological and Geochemical Characteristics and Metallogenic Mechanism of Aluminium Multi-Metal Deposits in Western Guangxi[J].Journal of Earth Sciences and Environment,2007,29(4):345-350.
Authors:DAI Ta-gen  LONG Yong-zhen  ZHANG Qi-zuan  HU Bin
Abstract:Some primary and cumulated types of aluminum multi-metal deposits occur in Western Guangxi region,and there is a close relationship between these two types of deposits.Some samples from the bauxites and wall-rocks are collected and tested for minor elements.It is shown that the metallogenic parent rocks for primary aluminum multi-metal deposits are Maokou Formation limestone of Lower Permian Series with a few of weathering of old land.The primary bauxite was formed in a marine sedimentary setting and the cumulated bauxite was derived from weathering-leaching of primary bauxite.
Keywords:aluminum multi-metal deposits  minor elements  geochemistry  metallogenic mechanism  Western Guangxi
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