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机构地区:[1]浙江省遂昌金矿
出 处:《黄金》1994年第10期6-13,共8页Gold
摘 要:本文通过银坑山金银矿床区域构造背景,基底构造和盖层构造分析,论述了该矿床的导矿、容矿、破矿构造特征和成矿关系,成矿前、成矿期、成矿后构造演化规律;建立了银坑山式金银矿床的构造控矿模式。Through analyses of regional tectonic background and tectonics of basement and covering strata of Yin-Keng-Shan Gold-Silver Deposit, the characteristics of the tectonics of magma hydrothermal passageway, magma hydrothermal deposition and posteriori mineralizatim as well as their relations with mineralization are described.In addition,the regularity of tectonic evoluation in the period of mineralization, priori and Posteriori mineralization are also expounded.The model of tectonic ore control of this deposit is established.
分 类 号:P618.510.2[天文地球—矿床学]
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