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Geochronological and genetic characterization of basaltic basement from western offshore basins in India
Abstract
40 Ar- 39 Ar geochronology, geochemistry, and Sr-Nd isotopic compositions of 30 core samples from 24 offshore drill wells in the Western offshore basins have been used to characterize the genetics of the volcanic basement from the Kutch, Mumbai, and Kerala-Konkan offshore basins. Findings from the volcanic basement rocks demonstrate extremely varied isotopic and geochemical fingerprints, which are suggestive of significantly diverse parent magma compositions and emplacement processes. Basaltic tholeiitic basement from Kutch Offshore basin has Ar-Ar ages that range between 60 Ma and 62 Ma. This basement is characterised by a within-plate basalt signature, with depleted isotopic signatures similar to least contaminated Deccan Traps basalts, and a component of subducted crustal material. Basaltic basement from Mumbai Offshore Basin has eruption ages between 63 Ma and 65 Ma and show a strong within-plate OIB affinity. Geochemical and isotopic signatures are consistent with Renuion lavas and an enriched-end member of Deccan Traps basalts. However, Kerala-Konkan Offshore Basin shows significant E-MORB affinity and is characterized by primitive-mantle signatures and least contamination from the upper continental crust, with ages of eruption between 60 Ma and 61 Ma based on obtained 40 Ar- 39 Ar ages. The study suggests that the Mumbai Offshore Basalts’ mode of the eruption was comparable with onshore Deccan volcanism, whereas the basaltic basement in Kutch Offshore was formed after…
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“Late volcanics and associated intrusives (63.0 ± 2.0 Ma) are exposed only in a small coastal strip around Mumbai (Maharashtra, India; clubbed into the Bombay Subgroup) but extend offshore to the Laxmi basin across the Arabian Sea (Fig. 1).”
From Spatio-temporal volume recalibration shows Deccan volcanism caused Terminal Cretaceous Mass Extinction (2026) · cites this paper as Gupta et al., 2024
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“They are synchronous with the India-Seychelles separation along the western margin of India (Pande et al., 2017b;Samant et al., 2019;Gupta et al., 2024).”
From Spatio-temporal volume recalibration shows Deccan volcanism caused Terminal Cretaceous Mass Extinction (2026) · cites this paper as Gupta et al., 2024
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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
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- Gupta, P., Rathore, S. S., & Singh, S.
- Venue
- Geoscience Frontiers
- Publisher
- Elsevier BV
- Published
- 2024-09
- Volume
- 15
- Issue
- 5
- Pages
- 101871
- ISSN
- 1674-9871
- Cited by
- 5
- References
- 2
- Language
- en
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- Oil and Natural Gas Corporation
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