| 东坡矿田蛇形坪铅锌矿床地质特征及成矿条件分析 |
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| 引用本文： | 孙振家,叶远荣.东坡矿田蛇形坪铅锌矿床地质特征及成矿条件分析[J].中南大学学报(自然科学版),1986(2). |
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| 作者姓名： | 孙振家 叶远荣 |
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| 作者单位： | 中南矿冶学院地质系，中南矿冶学院地质系 |
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| 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。
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| 关 键 词： | 矿源层 矿源体 构造位 |
GEOLOGICAL CHARACTERISTICS AND ANALYSES OF ORE--FORMING CONDITION IN THE SHEXINGPING LEAD--ZINC DEPOSIT OF DONPO METALLOGENETIC REGION |
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| Sun Zhenjia,Yie Yuanrong.GEOLOGICAL CHARACTERISTICS AND ANALYSES OF ORE--FORMING CONDITION IN THE SHEXINGPING LEAD--ZINC DEPOSIT OF DONPO METALLOGENETIC REGION[J].Journal of Central South University:Science and Technology,1986(2). |
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| Authors: | Sun Zhenjia Yie Yuanrong |
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| Institution: | Department of Geology |
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| 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. |
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| Keywords: | source beds metallogenetic body structural position |
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