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湘南铅锌矿床按传统分类,统属岩浆热液矿床。近年来,尹汉辉则将其分为两大类:即“与燕山期中酸性、酸性浅成-超浅成岩浆岩有关的岩浆期后热液矿床和与上古生代碳酸盐沉积建造有关的沉积-改造矿床”。笔者在本文中将前者称Ⅰ类,后者称Ⅱ类。 尹汉辉的分类除根据矿床的地质产状外,还着重考虑了铅、硫同位素组成特征和
According to the traditional classification, the lead-zinc deposits in the south of Hunan belong to the magmatic hydrothermal deposit. In recent years, Yin Hanhui has divided it into two categories: “post-magmatic post-magmatic deposits related to the acidic and acidic shallow-ultra-shallow magmatic rocks of the Yanshanian period and sediments associated with sedimentation of the Upper Paleozoic carbonate sediments - Transform the deposit. ” The author in this article will be the former class Ⅰ, the latter class Ⅱ. In addition to the classification of Yin Hanhui geological occurrence in the deposit, but also focused on the composition of the characteristics of lead and sulfur isotopes and