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攀——西地区基性超基性岩分布很广,岩体总数超过200个,其中部分岩体已经详勘或开采,是钒钛磁铁矿、铜镍(铂)硫化物矿产基地,同时有些超基性岩体有铬矿化现象。为了对其余岩体进行评价以及找寻深部矿体,我们参加了本区钒钛磁铁矿成矿规律与预测研究项目,对岩体的含矿性进行数学地质研究。现把研究成果作简要介绍,并对基性超基性岩含矿性数学地质研究中的几个问题提出一些粗浅的看法,供今后工作时参考。
Pan-West area of basic ultramafic rocks are widely distributed, the total number of rock more than 200, some of which have been detailed exploration or exploration of rock, vanadium titanomagnetite, copper nickel (platinum) sulfide mineral base, at the same time Some ultrabasic rocks have chrome mineralization. In order to evaluate the remaining rock mass and find out the deep orebody, we participated in the research project of the metallogenic regularity and prediction of vanadium-titanium magnetite in this area, and carried out mathematical geology research on the ore-bearing of the rock mass. Presently, the research results are briefly introduced, and some superficial opinions are put forward on several issues in the study of the basic ultramafic rock mineralization mathematical geology for reference when working in the future.