Deep dynamics and surface expression of the transition from oceanic subduction to continental collision

Published: 23-08-2019| Version 1 | DOI: 10.17632/ncvczg2myf.1
Hongrui Zhang


Figures S1 and S2 present Cathodoluminescence (CL) images and Chondrite normalized REE patterns of representative zircons. Figure S3 presents oxygen fugacities for the Paleocene magmatic rocks of the Gangdese belt. Table S1 presents age data for the Permo-Triassic magmatic rocks and HP metamorphic rocks of north-central Tibet. Tables S2 to S6 present the analytical results for whole-rock major- and trace-element and Nd isotopic analysis and zircon U–Pb dating and Hf isotopic analysis.