We present from the Lower Vindhyan Group, for the 𝗙𝗜𝗥𝗦𝗧 𝗧𝗜𝗠𝗘, compelling field evidence like buckle folds, reverse faults, and pop-up structures, commonly encountered in fold-thrust belts, that unambiguously support their collisional origin as opposed to the largely believed syn-sedimentary origin.

Last Friday was great! 😀

I got to talk about geology and my research to the enthusiastic 𝗝𝗦𝗣𝗦 𝗦𝗰𝗶𝗲𝗻𝗰𝗲 𝗗𝗶𝗮𝗹𝗼𝗴𝘂𝗲 𝗣𝗿𝗼𝗴𝗿𝗮𝗺 participants at the Kagawa Chuo High School. 🧑‍🔬🌏🗾🎌

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This study characterizes the origin of the ultra-high pressure Tso Morari Complex using whole-rock geochemical analyses and U-Pb geochronology. The Zircon U-Pb SHRIMP dates from the granite gneisses, eclogites, and amphibolites, along with conspicuous signatures of ...

📢📢 New Publication (Open Access)

Happy to share our newest publication from the Indian Ladakh Himalaya.

doi.org/10.1017/S001...