Calcium-O-Sr-Nd isotope evidence for the origin of REE-bearing carbonatite from metasomatized lithospheric mantle without recycled carbonate
Published: 30 May 2025| Version 3 | DOI: 10.17632/w23d2wss7g.3
Contributors:
Xing-Hui Li, Ming-Cai Xie, Kui-Feng Yang, Kan Li, chunming Han, Hai-Dong She, Gai-Zhong Liang, Xiao-Chun Li, Hongrui FanDescription
The data present comprehensive results of bulk-rock and in-situ mineral (olivine, apatite, calcite, and dolomite) major, trace elements, and Ca-O-Sr-Nd isotopes for the Qieganbulake carbonatite, located at the northeastern margin of the Tarim craton
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Institutions
- Institute of Geology and Geophysics Chinese Academy of SciencesBeijing, Beijing
Categories
Geology, Economic Geology, Petrology
Funders
- Ministry of Science and Technology of the People's Republic of ChinaBeijing, ChinaGrant ID: 2021YFC2901704