Article ID Journal Published Year Pages File Type
4573876 Geoderma 2012 20 Pages PDF
Abstract
► 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.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
Paleoweathering and depositional conditions in the inter-flow sediment units (bole beds) of Deccan Volcanic Province, India: A mineral magnetic approach
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