We further propose that these structures resulted from the Mesoproterozoic convergence between the Bundelkhand and Bastar Cratons along the Central Indian Tectonic Zone.

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.

We further propose that these structures resulted from the Mesoproterozoic convergence between the Bundelkhand and Bastar Cratons along the Central Indian Tectonic Zone.

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.

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It should not escape our attention as to how few FRS are women (11%!), but yet it took a woman to set an example.

royalsociety.org/-/media/poli...

thank you so much! 😊

Hi! Could you please add me to this one? Thanks! 😊