| 广东凡口铅锌(银)矿床成矿流体来源研究 |
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| 引用本文： | 张术根,周建普,黄满湘,樊钟衡.广东凡口铅锌(银)矿床成矿流体来源研究[J].矿产与地质,2002,16(4):199-202. |
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| 作者姓名： | 张术根 周建普 黄满湘 樊钟衡 |
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| 作者单位： | 中南大学资源环境与建筑工程学院地质研究所,湖南,长沙,410083 |
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| 摘 要： | 在已有研究成果的基础上 ,通过对矿物流体包裹体化学成分和氢氧同位素地球化学的研究 ,认为凡口矿区成矿期热液为多源混合流体 ,其来源包括建造水和岩浆水。这种混合流体的加热驱动与岩浆事件有关。
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| 关 键 词： | 流体包裹体 化学成分 氢氧同位素 流体来源 广东凡口铅锌矿 |
| 文章编号： | 1001-5663(2002)04-0199-04 |
| 修稿时间： | 2002年3月12日 |
THE ORIGIN OF ORE-FORMING FLUID OF FANKOU Pb、Zn(Ag)DEPOSIT,GUANGDONG |
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| ZHANG Shu gen,ZHOU Jian pu,HUANG Man xiang,FAN Zhong heng.THE ORIGIN OF ORE-FORMING FLUID OF FANKOU Pb、Zn(Ag)DEPOSIT,GUANGDONG[J].Mineral Resources and Geology,2002,16(4):199-202. |
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| Authors: | ZHANG Shu gen ZHOU Jian pu HUANG Man xiang FAN Zhong heng |
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| Abstract: | The Origin of ore forming fluid is one of the hotly debated problems about the genesis of Fankou Pb?Zn(Ag)deposit.On the basis of their former studies,the authors try to discuss this problem focused specially on the chemical and oxygen and hydrogen isotopoc compositions of fluid inclusions.The results suggest that the ore forming fluid is the mixture of magmatic fluid and deeply evoluted formational fluid driven by the thermal event in early Yanshanian granitic magmatic intrusion. |
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| Keywords: | fluid inclusions chemical compositions oxygen and hydrogen isotopes fluid origin Guangdong Fankou Pb Zn (Ag)deposit |
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