| 大营子金矿床成矿物理化学条件研究 |
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| 引用本文： | 姚玉增,梁俊红,金成洙,王建国.大营子金矿床成矿物理化学条件研究[J].地质找矿论丛,2001,16(1):32-37,57. |
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| 作者姓名： | 姚玉增 梁俊红 金成洙 王建国 |
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| 作者单位： | 东北大学 资源与土木工程学院, |
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| 摘 要： | 在详细研究大营子金矿床成矿地质背景及包裹体特征的基础上，利用化学热力学原理，对成矿流体的物理化学性质进行了计算，成矿溶液的氢氧同位素组成表明成矿流体为合来源，为先期深源岩浆热液叠加了后期雨水所致。
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| 关 键 词： | 成矿流体 物理化学条件 金矿床 成矿地质 流体包裹体 氢同位素 氧同位素 |
| 文章编号： | 1001-1412(2001)01-0032-06 |
| 收稿时间： | 2000/8/4 0:00:00 |
| 修稿时间： | 2001/1/2 0:00:00 |
STUDY ON THE METALLOGENIC PHYSI-CHEMICAL CONDITIONS OF DAYINGZI GOLD DEPOSIT |
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| YAO Yu-zeng,LIANG Jun-hong,JIN Cheng-zhu and WANG Jian-guo.STUDY ON THE METALLOGENIC PHYSI-CHEMICAL CONDITIONS OF DAYINGZI GOLD DEPOSIT[J].Contributions to Geology and Mineral Resources Research,2001,16(1):32-37,57. |
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| Authors: | YAO Yu-zeng LIANG Jun-hong JIN Cheng-zhu and WANG Jian-guo |
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| Institution: | Institute of Resource & Civil Engineering, Northeastern University, Shenyang 110006, China;Institute of Resource & Civil Engineering, Northeastern University, Shenyang 110006, China;Institute of Resource & Civil Engineering, Northeastern University, Shenyang 110006, China;Institute of Resource & Civil Engineering, Northeastern University, Shenyang 110006, China |
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| Abstract: | On the basis of detail analysis of ore forming geological background and characteristics of fluid inclusions, physi chemical conditions of the fluid inclusions are calculated. The composition of H O isotope indicates that the fluid originates from mixed resources; i.e.former magmatic water mixed with the later subterranean halogenic water. |
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| Keywords: | Dayingzi gold deposit ore forming fluid physi chemical conditions |
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