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Reappraisal of Duration and Eruptive Rates in Deccan Volcanic Province, India
Abstract
Rapidly expanding geochronological, paleomagnetic and volcanological data of the Deccan Volcanic Province (DVP) has given new insights to the expansive knowledge on it that had been built up through the preceding decades. Precursory Late Cretaceous (80 – 68 Ma) magmatic activity across the Indian subcontinent preceded the main event of volcanism. The main Deccan event involved nearly continuous outpourings of ~1.5 million km3 of flood basalts in a span of less than 2 m.y. on either side of the Cretaceous-Paleocene Boundary (KPB), corresponding to 3 magnetic chrons. This was followed by basaltic and silicic flows and alkaline magmatism that continued up to ~61 Ma. Several earlier postulated long-distance correlations of lava sequences based on chemical parameters are rendered invalid by the precision geochronology, leading to doubts regarding earlier models of volumetric eruptive rates. We suggest that pending better flow-field maps and correlations across the province, stacking rates based on thickness between chronological sampling points, combined with volcanological parameters provide a more robust and reproducible estimates of the eruptive rates. The stacking rates in different parts of the province were largely in the magnitude range of 103 m/m.y. and are comparable to those observed in other continental flood basalt provinces.
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“The morphological similarities of the Maastrichtian Malwa lavas with the Wai lavas (Kale et al., 2022) demonstrate that morphological character of the lavas and implicit eruptive rates (Kale and Pande, 2022) were not chronologically unique in the DVP, as inferred earlier.”
From Spatio-temporal volume recalibration shows Deccan volcanism caused Terminal Cretaceous Mass Extinction (2026) · cites this paper as Kale et al., 2022
In the citing paper
“The morphological similarities of the Maastrichtian Malwa lavas with the Wai lavas (Kale et al., 2022) demonstrate that morphological character of the lavas and implicit eruptive rates (Kale and Pande, 2022) were not chronologically unique in the DVP, as inferred earlier.”
From Spatio-temporal volume recalibration shows Deccan volcanism caused Terminal Cretaceous Mass Extinction (2026) · cites this paper as Kale and Pande, 2022
In the citing paper
“Kale and Pande (2022) and Pattabhiram et al. (2022) conclude that it is more apt to consider the Poladpur Formation as Danian lavas.”
From Spatio-temporal volume recalibration shows Deccan volcanism caused Terminal Cretaceous Mass Extinction (2026) · cites this paper as Kale and Pande, 2022
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U-Pb constraints on pulsed eruption of the Deccan Traps across the end-Cretaceous mass extinction
Schoene, B., Eddy, M. P., Samperton, K. M., Keller, C. B., Keller, G., Adatte, T., & Khadri, S. F. R. (2019) · Science · doi:10.1126/science.aau2422 · Cited by 542
The eruptive tempo of Deccan volcanism in relation to the Cretaceous-Paleogene boundary
Sprain, C. J., Renne, P. R., Vanderkluysen, L., Pande, K., Self, S., & Mittal, T. (2019) · Science · doi:10.1126/science.aav1446 · Cited by 395
Self-citationTriggering of the largest Deccan eruptions by the Chicxulub impact
Richards, M. A., Alvarez, W., Self, S., Karlstrom, L., Renne, P. R., Manga, M., Sprain, C. J., Smit, J., Vanderkluysen, L., & Gibson, S. A. (2015) · Geological Society of America Bulletin · doi:10.1130/b31167.1 · Cited by 210
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Cited by
Kale, V. S., Upasani, D., Rajput, M., Dole, G., & Pillai, S. P. (2026) · Geological Society of America Bulletin · doi:10.1130/b38412.1 · Cited by 3
Self-citation
Metadata
- Authors
- Kale, V. S., & Pande, K.
- Affiliations
- (Advanced Center for Water Resources Development and Management (ACWADAM) 1 , Kshipra Society, Pune - 411 058, India
- Department of Earth Sciences, Indian Institute of Technology (Bombay) 2 , Powai, Mumbai - 400 078, India
- Venue
- Journal of the Geological Society of India
- Publisher
- Geological Society of India
- Published
- 2022-01-01
- Volume
- 98
- Issue
- 1
- Pages
- 7-17
- ISSN
- 0974-6889
- 0016-7622
- Cited by
- 21
- References
- 4
- Language
- en
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