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东坡矿田蛇形坪铅锌矿床地质特征及成矿条件分析

GEOLOGICAL CHARACTERISTICS AND ANALYSES OF ORE--FORMING CONDITION IN THE SHEXINGPING LEAD--ZINC DEPOSIT OF DONPO METALLOGENETIC REGION

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【作者】 孙振家叶远荣

【Author】 Sun Zhenjia;Yie Yuanrong (Department of Geology)

【机构】 中南矿冶学院地质系中南矿冶学院地质系

【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.

【关键词】 矿源层矿源体构造位
【Key words】 source bedsmetallogenetic bodystructural position.
  • 【文献出处】 中南矿冶学院学报 , 编辑部邮箱 ,1986年02期
  • 【被引频次】3
  • 【下载频次】60
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