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新疆萨尔托海铬铁矿床是1958年发现的,前人曾进行过大量地质工作。提据地矿部“六五”期间对西准噶尔地区重要研究项目的要求,为探讨区域成矿特征,扩大矿床远景,从1982年起,魏文中工程师等四人对其进行专题研究。在分析整理前人大量勘探和科研成果的基础上,通过野外实地勘查和综合研究,运用一些新的研究手段,发现了造矿铬尖晶石中存在硅酸盐熔体包裹体,首次提出褪色岩石中富含氯硼、硫等挥发组分,认为这与铬矿成矿在空间上和成因上有密切关系。依据岩相、构造、己知矿体和岩石褪色带的分布、产状、划分了成矿带。阐述了各带成矿特征及其分市规律,提出在岩体中段有六个深部找矿地段。
The Salto Sea chromite deposit in Xinjiang was discovered in 1958, and many predecessors have carried out a large amount of geological work. In light of the requirements of important research projects in the West Junggar region during the “6th Five-Year Plan” period of the Ministry of Geology and Mines, in order to discuss the regional mineralization features and expand the prospect of the deposits, since 1982, Wei Wenzhong and other four engineers conducted special studies on them. On the basis of analyzing and researching a great deal of exploration and scientific research achievements of predecessors, through field investigation and comprehensive research in the field, and using some new research methods, it was found that the existence of silicate melt inclusions in the chromite of the ore making and the first fading The rock is rich in chlorine and boron, sulfur and other volatile components, that the chromium ore mineralization in space and genesis are closely related. Based on the lithofacies, tectonics, the distribution of known fossil ore bodies and faded zones of rock, and the occurrences, the metallogenic belt is divided. The metallogenic characteristics of each belt and the law of its subdivision are expounded. It is proposed that there are six deep ore prospecting sections in the middle of the rock mass.