中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Fluid evolution and ore genesis of the Tiantangshan granite-related vein-type Rb-Sn-W deposit, south China: constraints from LA-ICP-MS analyses of fluid inclusions

文献类型:期刊论文

作者Peng, Hong-Wei3,5; Fan, Hong-Rui1,3; Lecumberri-Sanchez, Pilar2; Lai, Jian-Qing5; Hu, Huan-Long3,4; Lan, Ting-Guang1,4; Li, Xing-Hui3
刊名MINERALIUM DEPOSITA
出版日期2022-12-12
页码19
ISSN号0026-4598
关键词LA-ICP-MS microanalyses Infrared microthermometry Fluid mixing Granite-related vein-type deposit Tiantangshan Rb-Sn-W deposit
DOI10.1007/s00126-022-01155-7
英文摘要Tungsten-tin-(rare-metal) deposits are most commonly granite-related and an important source of critical metals. This study describes the fluid evolution in the Tiantangshan Rb-Sn-W deposit, Nanling Range, China, and discusses the implications for mineralizing processes. Mineralization at Tiantangshan is spatially zoned. The greisen roof hosts wolframite-cassiterite quartz veins. The surrounding volcanic rocks host biotite quartz veins (Rb mineralization) crosscut by cassiterite quartz veins and sphalerite-galena quartz veins. The earliest intermediate-density fluids are responsible for the early W-(Sn)-Rb mineralization and evolve towards decreasing homogenization temperature (Th) and ratios of W, Sn, Rb, Cs, Fe, and Mn to Na + K as the fluid migrated from the greisen to the volcanic rocks hosted veins (Th: 420 to 350 degrees C; salinity: 13 to 4 wt% NaCleq). The spatial distribution of mineralization and fluid paragenesis indicates that precipitation of wolframite, early cassiterite, and Rb-rich biotite was associated with a pH increase during fluid-rock interaction. Late cassiterite and intergrown quartz precipitated from a degassing fluid with lower Th (mainly 360 to 340 degrees C) and salinity (10 to 2 wt% NaCleq) and with distinctly lower Sn concentrations. Late cassiterite precipitation is therefore likely related with depressurization by brittle failure of the rock leading to simultaneous boiling and meteoric water input. Late Pb-Zn mineralization precipitated from low Th (<320 degrees C) and salinity (0 to 2 wt% NaCleq) fluids through extensive mixing with meteoric water. The tempo-spatial development of Rb-Sn-W-Pb-Zn mineralization at Tiantangshan was controlled by a mixing fluid regime, where input of meteoric water gradually increased with time.
WOS关键词MAGMATIC-HYDROTHERMAL FLUIDS ; KEMPTVILLE TIN DEPOSIT ; COEXISTING WOLFRAMITE ; TUNGSTEN DEPOSITS ; JIANGXI PROVINCE ; ROCK INTERACTION ; QUARTZ ; INSIGHTS ; CASSITERITE ; MINERALIZATION
资助项目National Key Research and Development Program of China ; [2018YFA0702603]
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
出版者SPRINGER
WOS记录号WOS:000898326800001
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/106951]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Fan, Hong-Rui
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
2.Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
4.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550081, Peoples R China
5.Cent South Univ, Minist Educ, Sch Geosci & Info Phys, Key Lab Metallogen Predict Nonferrous Met & Geol E, Changsha 410083, Peoples R China
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Peng, Hong-Wei,Fan, Hong-Rui,Lecumberri-Sanchez, Pilar,et al. Fluid evolution and ore genesis of the Tiantangshan granite-related vein-type Rb-Sn-W deposit, south China: constraints from LA-ICP-MS analyses of fluid inclusions[J]. MINERALIUM DEPOSITA,2022:19.
APA Peng, Hong-Wei.,Fan, Hong-Rui.,Lecumberri-Sanchez, Pilar.,Lai, Jian-Qing.,Hu, Huan-Long.,...&Li, Xing-Hui.(2022).Fluid evolution and ore genesis of the Tiantangshan granite-related vein-type Rb-Sn-W deposit, south China: constraints from LA-ICP-MS analyses of fluid inclusions.MINERALIUM DEPOSITA,19.
MLA Peng, Hong-Wei,et al."Fluid evolution and ore genesis of the Tiantangshan granite-related vein-type Rb-Sn-W deposit, south China: constraints from LA-ICP-MS analyses of fluid inclusions".MINERALIUM DEPOSITA (2022):19.

入库方式: OAI收割

来源:地质与地球物理研究所

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