上坪钨矿床成因分析

Z. Gan
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引用次数: 0

摘要

每个矿床的形成都有其客观条件和自然条件。不同的矿床因其形成的条件和环境不同而具有不同的类型。本文对上坪钨矿的成因进行了分析和探讨。首先是区域背景。其次是矿床的地质特征和年龄。从整个发育过程来看,认为该矿床为伟晶岩岩相向热液溶蚀阶段逐渐间歇逆沉淀的分带矿床。从矿床特征看,这是一个较为复杂的(FeMn) WO4 -石英高温热液矿床,具有细脉型。从不同的角度进行原因分类是本文的新颖之处。其目的是了解钨矿的分布规律,为指导矿山生产和找矿服务。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Cause-Forming Analysis of Shangping Tungsten Deposit
The forming of each deposit has its objective and natural conditions. Different deposits have different types because their conditions and environments are different. This paper analyzed and discussed the cause of Shangping tungsten deposit. Firstly, it is the district background. Secondly, it is the geological characteristics and the age of the deposit. We think that the deposit is the zoning deposit of intermittently reverse precipitation from the pegmatite petrography to the hydrothermal solution stage gradually from the whole developing process. And this is a more complicated high temperature hydrothermal solution deposit of (FeMn) WO4 and quartz with thin-vein type from the characteristics of the deposit. The cause classification from different was is new and original in the paper. Its aim is to finding out the distribution regulation of the tungsten deposit and to serve for directing mine production and prospecting bitterly.
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