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Variation of melting processes and magma sources of the early Deccan flood basalts, Malwa Plateau, India
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“The majority of lavas with the lowest values of Ba/Nb overlap with Reunion ocean island hot-spot basalt compositions (Haase et al., 2019) and erupted quasi-continuously over a period of ∼350,000 years (Figure 3).”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Haase et al., 2019
In the citing paper
“Alkaline compositions at the base of exposed sections erupted within Chron 30N (Haase et al., 2019;Schöbel et al., 2014) and assuming accurate placement of the Chron 30N/29R boundary by Schöbel et al. (2014), the transition to solely tholeiitic compositions occurs after the first 500,000 years of eruptions.”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Haase et al., 2019
In the citing paper
“Overall, our major, minor, and trace element data overlap substantially with those of Haase et al. (2019) for the Malwa Plateau (Figure 4).”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Haase et al., 2019
In the citing paper
“However, Sr-Nd-Pb isotopic compositions of at least some of the Malwa basalts (Haase et al., 2019;Marzoli et al., 2022;Peng et al., 1998) are depleted (e.g., yield positive epsilon Nd values) and generally similar to those of Wai basalts from the Western Ghats.”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Haase et al., 2019
In the citing paper
“However, the two groups of contaminated basalts are clearly distinct in terms of Pb isotopic compositions (Basu et al., 2020;Haase et al., 2019;Peng et al., 1998), suggesting that they were contaminated by distinct crustal rocks.”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Haase et al., 2019
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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
Triggering 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
The Magmatic Architecture of Continental Flood Basalts I: Observations From the Deccan Traps
Mittal, T., Richards, M. A., & Fendley, I. M. (2021) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2021jb021808 · Cited by 42
Tholt, A. J., Renne, P. R., Marzoli, A., Vanderkluysen, L., Mohabey, D., Samant, B., Dhobale, A., Pande, K., & Self, S. (2023) · Geochemistry, Geophysics, Geosystems · doi:10.1029/2023gc011137 · Cited by 15
Metadata
- Authors
- Haase, K. M., Regelous, M., Schöbel, S., Günther, T., & de Wall, H.
- ORCID
- Haase, K.M.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2019-10
- Volume
- 524
- Pages
- 115711
- ISSN
- 0012-821X
- Cited by
- 23
- References
- 3
- Language
- en
- Funders
- Friedrich-Alexander-Universität Erlangen-Nürnberg
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