Paleoweathering and depositional conditions in the inter-flow sediment units (bole beds) of Deccan Volcanic Province, India: A mineral magnetic approach

► We study origin of Fe-oxides in inter-flow units (boles) of Deccan Volcanism. ► Colored boles characterize depositional environments and magnetic mineralogy. ► Baking, surface run-off, infiltration and ponding are prevalent. ► Contributes to post eruptive environments and study of Martian soils.