东坡矿田蛇形坪铅锌矿床地质特征及成矿条件分析

来源期刊：中南大学学报(自然科学版)1986年第2期

论文作者：孙振家 叶远荣

文章页码：7 - 13

关键词：矿源层； 矿源体； 构造位

Key words：source beds； metallogenetic body； structural position.

摘    要：本矿床产于花岗斑岩与碳酸盐岩接触带,前人认为单一岩浆热液成因。经我们对矿床地质特征综合研究,提出应为矿源层、矿源体、构造位三个成矿条件综合控制形成的矿体。本文总结这类地质特征及成矿条件,不但在理论上而且在本区实际上也具有意义。

Abstract: The metallogenetic region of Shexingping lead-zinc deposit occures in the contact zone of granite and carbonatite. The former scholars considered it as a magmatic-hydrothermal deposit. Based on the synthetical study of the characteristics of the deposit, we regard it as a deposit which is formed under the synthetic control of the three ore-forming conditions: source beds metallogenetic body and structural position. So no matter whether in practice or in theroy, it is very significant to summarize the geological characteristics and ore-forming condition of this kind of deposits.