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| 湖南瑶岗仙钨矿床成矿流体演化特征研究 | |
| 引用本文： | 于志峰,许虹,祝新友,王艳丽,程细音.湖南瑶岗仙钨矿床成矿流体演化特征研究[J].矿床地质,2015,34(2):309-320. |
| 作者姓名： | 于志峰 许虹 祝新友 王艳丽 程细音 |
| 作者单位： | 1. 中国地质大学地球科学与资源学院,北京100083;北京矿产地质研究院,北京 100012 2. 中国地质大学地球科学与资源学院,北京,100083 3. 北京矿产地质研究院,北京 100012;中色地科矿产勘查股份有限公司,北京 100012 4. 有色金属矿产地质调查中心,北京,100012 5. 中色地科矿产勘查股份有限公司,北京,100012 |
| 基金项目： | 本文得到国家科技支撑课题项目"湖南锡田地区深部成矿岩体空间结构与成矿预测(批准号: 2011BAB04B08)"、老矿山深部和外围找矿项目"湖南省桂阳县黄沙坪铅锌矿接替资源勘查(批准号:资[2013]01-036-049)"的资助 |
| 摘 要： | 瑶岗仙矿床位于湖南省郴州市瑶岗仙镇,是世界著名的钨矿床。近几年,随着云英岩析离体的发现,对于成矿流体的演化过程有了新的认识。文章通过对瑶岗仙石英脉型黑钨矿矿床的中粒碱长花岗岩、云英岩析离体和石英脉3个阶段地质体的石英中的流体包裹体进行显微测温和激光拉曼光谱分析,并对云英岩析离体中的熔流包裹体进行加热熔化实验,初步证明了瑶岗仙矿床石英脉型黑钨矿阶段成矿流体的演化是由花岗质岩浆→浆液过渡态岩浆→岩浆热液的一个完整连续的过程,而且成矿流体以富含挥发分为特征。并结合地质现象,提出浆液过渡态流体与成矿作用具有直接联系。 |
| 关 键 词： | 地球化学 流体包裹体 熔流包裹体 熔融包裹体 成矿流体演化 瑶岗仙钨矿床 |
| 收稿时间： | 1/9/2014 12:00:00 AM |
| 修稿时间： | 2015/3/10 0:00:00 |
Characteristics and evolution of ore-forming fluids in Yaogangxian tungsten deposit, Hunan Province |
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| YU ZhiFeng,XU Hong,ZHU XinYou,WANG YanLi and CHENG XiYin.Characteristics and evolution of ore-forming fluids in Yaogangxian tungsten deposit, Hunan Province[J].Mineral Deposits,2015,34(2):309-320. | |
| Authors: | YU ZhiFeng XU Hong ZHU XinYou WANG YanLi and CHENG XiYin |
| Institution: | School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;Beijing Institute of Geology for Mineral Resources, Beijing 100012, China;School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;Beijing Institute of Geology for Mineral Resources, Beijing 100012, China;Sinotech Mineral Exploration Co., Ltd., Beijing 100012, China;China Non-ferrous Metals Resource Geological Survey, Beijing 100012, China;Sinotech Mineral Exploration Co., Ltd., Beijing 100012, China |
| Abstract: | Located at Yaogangxian Town in Chenzhou City of Hunan Province, the Yaogangxian deposit is one of the most famous tungsten deposits in China. Recently, with the discovery of segregation bodies of greizen, some new understanding concerning the evolutionary process of ore-forming fluids in the Yaogangxian deposit has been obtained. This paper focuses on the study of inclusions in quartz from three evolution stages in the Yaogangxian deposit, during which medium grained alkali feldspar granite, greizen segregation body and quartz veins were formed, respectively. The results of the microthermometric experiments and laser Raman spectroscopy on fluid inclusions of quartz and heating-melting experiments on fluid-melt inclusions of greizen segregation bodies indicate that a complete successive evolutionary process of the ore-forming fluids in the Yaogangxian deposit actually evolved from granitic lava state through lava-fluid transitional state to magmatic hydrothermal state, and the ore-forming fluids were rich in volatiles. Combined with geological background, the authors hold that there existed the direct relationship between the lava-fluid transitional fluid and the mineralization in the Yaoganxian deposit. |
| Keywords: | geochemistry fluid inclusions fluid-melt inclusions melt inclusions evolution of ore-forming fluids Yaogangxian tungsten deposit |
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