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 Sun

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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

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