Origin of clays in the interbasaltic red boles of Deccan Volcanics: pedogenesis versus palagonitization
Red-coloured clay-rich beds (bole beds) occur at flow breaks in parts of the Deccan volcanic province (DVP). These boles in the Deccan province retain paleoenvironmental information that prevailed at the K-T boundary, including the timing of the Deccan eruption synchronous with the K-T mass extincti...
| Main Authors: | , , , , |
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| Formato: | Journal article |
| Idioma: | English |
| Publicado em: |
Elsevier
2023
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