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 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
Files
Institutions
Institute of Geology and Geophysics Chinese Academy of Sciences
Categories
Geology, Economic Geology, Petrology
Funding
Ministry of Science and Technology of the People's Republic of China
2021YFC2901704