Geochronology and geochemistry of intrusion and multi-generation garnet at the Jia’erbasidao Fe skarn deposit: Implications for two-stage Fe mineralization in the Chinese Altay Orogen (NW China)-Reference-Cited by-同舟云学术

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Geochronology and geochemistry of intrusion and multi-generation garnet at the Jia’erbasidao Fe skarn deposit: Implications for two-stage Fe mineralization in the Chinese Altay Orogen (NW China)

Published:2023-12 Issue: Volume:163 Page:105777
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Zhang Xuebing^ORCID,Chai Fengmei,Xiao Bing,Chu Gaobin,Feng Yuzhou,Lai Chun-kit

Funder

National Natural Science Foundation of China

Ministry of Science and Technology of the People's Republic of China

National Key Research and Development Program of China

Natural Science Foundation of Xinjiang Uygur Autonomous Region

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference50 articles.

1. Rare-earth element mobility during hydrothermal and metamorphic fluid–rock interaction and the significance of the oxidation state of europium;Bau;Chem. Geol.,1991

2. Boynton, W.V., 1984. Geochemistry of the rare earth elements: Meteorite studies. Rare Earth Element Geochemistry (ed. P Henderson) 63-114.

3. Tectonic development of the southern Chinese Altai Range as determined by structural geology, thermobarometry, 40Ar/39Ar thermochronology, and Th/Pb ion-microprobe monazite geochronology;Briggs;Geol. Soc. Am. Bull.,2009

4. Geochemistry and geochronology of multi-generation garnet: New insights on the genesis and fluid evolution of prograde skarn formation;Chu;Geoscience Frontiers,2023

5. Dating magmatic and hydrothermal processes using andradite-rich garnet U-Pb geochronometry;Deng;Contrib. Mineral. Petrol.,2017

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