Supplemental Material: Metamorphic evolution and geochronology of the tectonic mélange of the Dongbatu and Mogutai blocks, middle Dunhuang orogenic belt, northwestern China
posted on 2018-04-01, 00:00authored byHao Y.C. Wang, Qian W.L. Zhang, Jun-Sheng Lu, Hong-Xu Chen, Jia-Hui Liu, Hui C.G. Zhang, Van Tho Pham, Tao Peng, Chun-Ming Wu
Geosphere, April 2018, v. 14, p. 883-906, doi:10.1130/GES01514.1, Supplemental Item B. Table S1: Chemical compositions of the representative minerals in the high-pressure mafic granulite, amphibolite, and metapelite from the Dongbatu and Mogutai blocks. Table S2: SIMS U-Pb isotopes of zircons from the granulite, amphibolite, and metapelite in the Dongbatu and Mogutai blocks. Table S3: LA-ICP-MS U-Pb isotopes of zircons from the metapelite in the Dongbatu and Mogutai blocks.