Transition from kinetic to equilibrium Zr isotope fractionations during magma crystallization
Published: 10 January 2024| Version 1 | DOI: 10.17632/sjz9jpmfy3.1
Contributors:
Zhen-Xin Li, Shao-Bing Zhang, Yong-Fei Zheng, Michael A. Antonelli, Wen Zhang, Liang Zhang, Ting Liang, Fang-Yuan SunDescription
This data contain all supplemantry materials associated with the manuscript: Transition from kinetic to equilibrium Zr isotope fractionations during magma crystallization.
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The Zr isotope compositions of zircon were measured by using a 257 nm Yb:YGB femtosecond laser ablation system connected to a Neptune MC-ICPMS. The Hf contents of zircon were measured by LA-ICPMS. All modelling were simulated by GeoPS and Rhyolite-MELTS.
Institutions
University of Science and Technology of China
Categories
Earth Sciences