Sulfide saturation in reduced magmas during generation of the Gangdese juvenile lower crust: Implications for porphyry Cu–Au mineralization in the Gangdese belt, Tibet

Name: Sulfide saturation in reduced magmas during generation of the Gangdese juvenile lower crust: Implications for porphyry Cu–Au mineralization in the Gangdese belt, Tibet
Creator: jinlei sun
Published: 2023-07-06T19:37:18.285Z
Keywords: Geochemistry

sun, jinlei; Bai, Zhong-Jie

doi:10.17632/bshzz7txvz.1

Sulfide saturation in reduced magmas during generation of the Gangdese juvenile lower crust: Implications for porphyry Cu–Au mineralization in the Gangdese belt, Tibet

Published: 6 July 2023| Version 1 | DOI: 10.17632/bshzz7txvz.1

Contributors:

jinlei sun, Zhong-Jie Bai

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LA-ICP-MS zircon U–Pb dating data, zircon Hf isotope, zircon trace element compositions, whole-rock major (wt.%) and trace element (ppm) compositions, estimated concentration of chalcophile elements are provided in Supplementary Tables S1-S6. Plots of PGEs, Au and Cu versus MgO, and S contents are included in Supplementary Figures S1-S2.

Sulfide saturation in reduced magmas during generation of the Gangdese juvenile lower crust: Implications for porphyry Cu–Au mineralization in the Gangdese belt, Tibet

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