【摘 要】
：
本文就所积累的岩石及矿石全分析以及岩矿(?)定资料,对某地超基性岩体中铬铁矿矿化问题作进一步探讨。一、岩体地质情况简介某超基性岩体位于黄陵台凸基底之西南部,受前震旦
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本文就所积累的岩石及矿石全分析以及岩矿(?)定资料,对某地超基性岩体中铬铁矿矿化问题作进一步探讨。一、岩体地质情况简介某超基性岩体位于黄陵台凸基底之西南部,受前震旦纪黄陵褶(?)区的北西西一南东东向断裂构造控制,走向北67°西,呈条带状分布,面积约14平方公
In this paper, the accumulated rock and ore analysis as well as rock and mineral ()) fixed data, further exploration into the mineralization of chromite in an ultramafic rock mass. I. INTRODUCTION TO GEOPHYSICAL CONDITIONS An ultrabasic rock mass is located in the southwestern part of the basement of the Huangling Platform and controlled by a north-west-south-east-east fault structure of the former Sinian Huangling fold (?) Region, heading north 67 ° West, was strip-shaped distribution, an area of about 14 square kilometers
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