Calcium-O-Sr-Nd isotope evidences for the origin of REE-bearing carbonatite from carbonate-metasomatized lithospheric mantle

Published: 20 February 2025| Version 2 | DOI: 10.17632/w23d2wss7g.2
Contributors:
Xing-Hui Li, Ming-Cai Xie, Kui-Feng Yang, Kan Li, chunming Han, Hai-Dong She, Gai-Zhong Liang, Xiao-Chun Li, Hongrui Fan

Description

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 Sciences

Categories

Geology, Economic Geology, Petrology

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