Subduction erosion revealed by Late Mesozoic magmatism in the Gangdese arc, South Tibet

Subduction erosion revealed by Late Mesozoic magmatism in the Gangdese arc, South Tibet

The supporting information includes the Analytical methods (Text S1), Figure S1 of LA-ICP-MS zircon U-Pb concordia diagrams with cathodoluminescence images in this study, Figure S2 of 87Sr/86Sr(i) versus ε Nd(t) diagram for Mesozoic mantle-derived magma, Figure S3 of Geochemical diagrams for Late Cr...

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Bibliographische Detailangaben
1. Verfasser: Huang, Tong-yu
Format: Dataset
Sprache:eng
Schlagworte:
FOS: Earth and related environmental sciences
Geology
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Zusammenfassung:The supporting information includes the Analytical methods (Text S1), Figure S1 of LA-ICP-MS zircon U-Pb concordia diagrams with cathodoluminescence images in this study, Figure S2 of 87Sr/86Sr(i) versus ε Nd(t) diagram for Mesozoic mantle-derived magma, Figure S3 of Geochemical diagrams for Late Cretaceous and pre-Late Cretaceous subduction-related adakitic rocks, Figure S4 of quantitative calculation of juvenile crust generation rate and tectonic erosion rate from Zedong and nearby area, and Tables S1-S8 of the analytical results.
DOI:10.6084/m9.figshare.19530532