黔中川主庙铝土矿矿床地质特征
Nonferrous Metals Abstract(2015)
Abstract
本文通过对川主庙铝土矿矿区含矿岩系岩性组合特征及其与顶底板之间的关系进行分析,结合古地理等情况,进一步证明了黔中川主庙铝土矿成矿物质来源主要来源于基底湄潭组、桐梓组泥页岩(少量来源于白云岩、灰岩)、及黔中铝土矿矿床成因为:“母岩风化剥蚀-原地堆积(部分搬运沉积)-进一步风化淋滤-成矿”的观点.
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