Molybdenum isotopes record dehydrated slab components input to arc magmatism in subduction zones

Published: 18 October 2024| Version 1 | DOI: 10.17632/3nx7kvk2hb.1
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金磊

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The Supplementary Material contains: Sr–Nd iThe Supplementary Material contains: Sr–Nd isotopes, Trace elements abundance in hornblendes, and Parameters of the mixing model (Table S1-S3). Representative photomicrographs of the Milin cumulates (Fig.S1); plot of Mo contents versus SiO2 (a), S (b), Fe2O3T (c) and TiO2 (d) (Fig.S2); plot of δ98/95Mo values versus SiO2 (a), Fe2O3T (b), TiO2 (c) and S (d) (Fig.S3); plot of (87Sr/86Sr)i, and εNd(t) values versus MgO (a–b) and δ98/95Mo (c–d) (Fig.S4); plot of LOI versus (87Sr/86Sr)i (a), εNd(t) (b) and δ98/95Mo (c) (Fig.S5).sotopes, Trace elements abundance in hornblendes, and Parameters of the mixing model (Table S1-S3). Representative photomicrographs of the Milin cumulates (Fig.S1); plot of Mo contents versus SiO2 (a), S (b), Fe2O3T (c) and TiO2 (d) (Fig.S2); plot of δ98/95Mo values versus SiO2 (a), Fe2O3T (b), TiO2 (c) and S (d) (Fig.S3); plot of (87Sr/86Sr)i, and εNd(t) values versus MgO (a–b) and δ98/95Mo (c–d) (Fig.S4); plot of LOI versus (87Sr/86Sr)i (a), εNd(t) (b) and δ98/95Mo (c) (Fig.S5).

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