Deep arc root cumulates and implication for crustal growth in the southern Central Asian Orogenic Belt

Figure S1 shows the photomicrographs of peridotite, pyroxenite, and gabbro from the Hongliuhe and Yushishan areas. Figure S2 showsAmphibole compositions. Figure S3 shows Zircon U-Pb concordia diagrams and cathodoluminescence (CL) images. Figure S4 shows primitive mantle normalized spider diagrams of the ultramafic rocks from the study areas.The major and trace element data of standards are listed in Table S1. The major elements of minerals from Hongliuhe and Yushishan are listed in Table S2-S6. Calculated temperature and pressure, zircon U-Pb age of gabbros, and differentiation simulation can be found in Table S7-S9.