Supplemental Material: Fluid-fluxed melting in the Himalayan orogenic belt: Implications for the initiation of E-W extension in southern Tibet

Abstract

<p>Supplemental Text S1: Analytical Methods. Figure S1: Cathodoluminescence (CL) showing the texture, spot, and respective age of zircon U-Pb dating for the leucogranites from the Cona and Everest regions along the Himalayan orogenic belt. Figure S2: U-Pb Concordia diagrams showing the crystallization ages of the representative leucogranites derived from fluid-absent melting (Group A) from the Cona and Everest regions along the Himalayan orogenic belt. Figure S3: Sr-Nd isotope systematics of the two types of leucogranites from the Malashan, Cona, and Everest regions along the Himalayan orogenic belt. Table S1: Summary of SHRIMP zircon U-Pb isotope data for the leucogranite in the Himalayan orogenic belt. Table S2: Summary of MC-ICP-MS zircon U-Pb isotope data for the leucogranite in the Himalayan orogenic belt. Table S3: Major and trace element compositions, as well as Sr-Nd isotope compositions of the leucogranite in the Himalayan orogenic belt.</p>