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一、矿床成因的几种认识内蒙狼山霍各乞是一有一定规模的铜铅锌多金属矿床,内蒙511队和研究所曾进行了普查勘探和科研工作。对于该矿床的成因,有以下几种不同的认识:一曰岩浆期后热液矿床(包括矽卡岩型和中温热液矿床);二曰同生沉积变质矿床(包括复生沉积变质和火山沉积变质矿床);三曰岩浆热液叠加层控变质矿床。笔者在前人工作的基础上,通过近年对霍各乞矿床的研究,认为该矿床虽表现有某些沉积特征,但不是同生沉积受变质矿床,它虽具热
First, the understanding of several causes of the deposit Huozu begging Inner Mongolia Wolf Hill is a certain size of the copper-lead-zinc polymetallic deposits, Inner Mongolia 511 team and the Institute conducted a survey and scientific research. There are several different understandings of the origin of the deposit: one is the post-magmatic hydrothermal deposit (including skarn-type and mid-temperature hydrothermal deposit); the other is the sedimentary metamorphic deposit (including the reactivation metamorphism and volcano Sedimentary metamorphic deposit); Third, superposition magmatic hydrothermal superimposed metamorphic deposits. Based on the work of predecessors, based on the work of the predecessors, the author thinks that although the deposit shows some sedimentary characteristics, it is not a sedimentary deposit of the same genesis. Although it is hot