Figure S1: Geological map of the Baijnath klippe showing the sample position used for petrological, geochemical, and geochronological study. Figure S2: Ti-versus-XMg plot of Ti-in-biotite of two textural modes. Figure S3: Wetherill plots of U-Pb zircon data for each sample: (A) mylonitic granitoids, (B) less-deformed granitoids, and (C) supracrustal rocks. Table S1: Representative mineral chemical data analyzed by EPMA from the samples of Baijnath supracrustals. Table S2: Mineral compositional data of amphibole along the Hbl-Bt profile. Table S3: Representative major and trace element data with CIPW norm data from the Baijnath granitoids. Table S4: Zircon U-Pb (LA-ICP-MS) data from the samples of the Baijnath klippe. Table S5: Apatite U-Pb (LA-ICP-MS) data from the samples of the Baijnath supracrustals. Table S6: Representative Ti-in-zircon, Ti-in-quartz thermometric data and pressure estimation data for the granitoids. Table S7: General description, modal abundance of the supracrustal samples used in this work.
No takes yet. Share an insight, caveat, or question.
Mukherjee et al. (2024) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: