Magmatic-hydrothermal evolution of an unusual Mo-rich carbonatite: a case study using LA-ICP-MS fluid inclusion microanalysis and He–Ar isotopes from the Huangshui’an deposit, Qinling, China-Reference-Cited by-同舟云学术

Magmatic-hydrothermal evolution of an unusual Mo-rich carbonatite: a case study using LA-ICP-MS fluid inclusion microanalysis and He–Ar isotopes from the Huangshui’an deposit, Qinling, China

Published:2021-04-20 Issue:6 Volume:56 Page:1133-1150
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Tang Li^ORCID,Wagner Thomas,Fusswinkel Tobias,Zhang Shou-Ting,Xu Bo,Jia Li-Hui,Hu Xin-Kai

Funder

Open Research Project from the State Key Laboratory of Geological Processes and Mineral Resources

National Key Research and Development Program of China

German Research Foundation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

https://link.springer.com/content/pdf/10.1007/s00126-021-01055-2.pdf

Reference92 articles.

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3. Anenburg M, Mavrogenes JA (2018) Carbonatitic versus hydrothermal origin for fluorapatite REE-Th deposits: experimental study of REE transport and crustal "antiskarn" metasomatism. Am J Sci 318:335–366

4. Anenburg M, Mavrogenes JA, Bennett VC (2020a) The fluorapatite P–REE–Th vein deposit at Nolans Bore: genesis by carbonatite metasomatism. J Petrol 61. https://doi.org/10.1093/petrology/egaa003

5. Anenburg M, Mavrogenes JA, Frigo C, Wall F (2020b) Rare earth element mobility in and around carbonatites controlled by sodium, potassium, and silica. Sci Adv 6. https://doi.org/10.1126/sciadv.abb6570

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