Data for: Magmatic recycling of accretionary wedge: a new perspective on Silurian-Devonian I-type granitoids generation in the Chinese Altai

Published: 31 March 2020| Version 1 | DOI: 10.17632/6ytpfd46j2.1
Yingde Jiang


The supplementary Fig. S1 is classification of Silurian-Devonian granitods in the Chinese Altai. Fig. S2, S3 and S4 are supplements to Fig. 6 to dispaly chemical changes of the modelled melts with increasing teperature at different pressures. Table S1 and S2 show some relevant data of the Ordovician Habahe Group rocks and Silurian-Devonian granitoids in the Chinese Altai. Table S3 is about some related melting modelled consequences. Table S4 illustrate the calculating processes of trace element modelling and data of used partition coefficients.