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| 蚀变粗面岩中再平衡结构黑云母的电子探针分析 | |
| 引用本文： | 聂潇,王宗起,陈雷,陈浦浦,王刚.蚀变粗面岩中再平衡结构黑云母的电子探针分析[J].岩矿测试,2019,38(5):565-574. |
| 作者姓名： | 聂潇 王宗起 陈雷 陈浦浦 王刚 |
| 作者单位： | 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室, 北京 100037,中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室, 北京 100037,中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室, 北京 100037,山西地矿海外工程建设有限公司, 山西 太原 030002,中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室, 北京 100037 |
| 基金项目： | 国家自然科学基金面上项目（41872092）；中国地质调查局地质调查项目“境外大型矿产资源基地及资源潜力评价”（DD20190437），“矿产资源国情调查数据集成与动态更新”（DD20190613） |
| 摘 要： | 黑云母的化学成分中蕴含着重要的成因信息,对具有交代结构的黑云母进行微区成分分析,能够精细反映交代蚀变过程中元素迁移情况,为解决矿床形成机制方面的科学问题提供矿物学证据。本文以北大巴山平利地区蚀变粗面岩中具有再平衡结构的黑云母斑晶为研究对象,进行电子探针面扫描和剖面成分分析。结果表明,斑晶内部为岩浆成因黑云母,边缘为"扩散-反应"过程所致的再平衡成因黑云母。斑晶边缘与内部相比,TiO_2含量由平均5.78%降至2.22%,表明在交代蚀变过程中黑云母中Ti等高场强元素被淋滤出进入流体;而CaO含量由平均0.06%升至0.14%,F含量由平均0.60%升至0.80%,指示蚀变流体内富含Ca、F等组分。本研究揭示了粗面岩中铌矿床的形成与热液作用关系密切,成矿流体中Ca、F等组分在铌元素的迁移及富集过程中具有重要作用。 |
| 关 键 词： | 黑云母 电子探针 再平衡结构 铌矿床 粗面岩 |
| 收稿时间： | 2018/7/10 0:00:00 |
| 修稿时间： | 2019/3/5 0:00:00 |
Electron Microprobe Analysis of Biotite with Reequilibration Texture in Altered Trachyte |
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| NIE Xiao,WANG Zong-qi,CHEN Lei,CHEN Pu-pu and WANG Gang.Electron Microprobe Analysis of Biotite with Reequilibration Texture in Altered Trachyte[J].Rock and Mineral Analysis,2019,38(5):565-574. | |
| Authors: | NIE Xiao WANG Zong-qi CHEN Lei CHEN Pu-pu and WANG Gang |
| Institution: | Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China,Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China,Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China,Shanxi Dikuang Overseas Engineering Construction Co. LTD, Taiyuan 030002, China and Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China |
| Abstract: | BACKGROUND:The chemical composition of biotite contains important genetic information. The in-situ analyses of biotite with metasomatic texture can reflect the migration of the elements during the metasomatic alteration, and provide mineralogical evidence for the ore-forming mechanism. OBJECTIVES:To investigate the migration of elements during trachyte alteration and reveal the Nb mineralization mechanism in altered trachyte. METHODS:Biotite phenocryst with reequilibration texture in altered trachyte in the Pingli area of North Dabashan was studied, and the EMPA element mapping and line profile analyses were carried out. RESULTS:The results show that the phenocryst was magmatic in the core and the reequilibrated origin on the rim, caused by diffusion-reaction process. Compared with the core, the TiO2 content decreased from an average of 5.78% to 2.22% in the rim, indicating that Ti was leached out into the fluid during the exchange alteration. The CaO content increased from 0.06% to 0.14% on average, and the F content increased from 0.60% to 0.80% on average, suggesting that the alteration fluid is rich in Ca and F. CONCLUSIONS:The formation of Nb deposits in trachyte is closely related to the hydrothermal activity, and the components such as Ca and F in the ore-forming fluid play an important role in the migration and enrichment of Nb. |
| Keywords: | biotite electron microprobe analysis reequilibration textures Nb deposit trachyte |
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