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Magnetostratigraphy and 40Ar–39Ar geochronology of the Malwa Plateau region (Northern Deccan Traps), central western India: Significance and correlation with the main Deccan Large Igneous Province sequences
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“If the subsurface extent of lavas around the Narmada Rift is near the upper inferred limit, the total present volume of Malwa lavas probably exceeds the amount estimated by Schöbel et al. (2014), who assumed an average thickness of 300 m.”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Schöbel et al., 2014
In the citing paper
“Some previous studies of Malwa basalts were focused on the paleomagnetic stratigraphy (e.g., Bhalla & Rao, 1974;Khadri, 2003;Khadri & Nagar, 1994;Schöbel et al., 2014) and revealed a normal-reverse-normal polarity sequence spanning Chrons 30N-29R-29N.”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Schöbel et al., 2014
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“The current areal extent and volume of the Malwa Plateau magmatic rocks are estimated to be 80,000 km 2 and 21,000 km 3 , respectively (Schöbel et al., 2014).”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Schöbel et al., 2014
In the citing paper
“Schöbel et al. (2014) used the anisotropy of magnetic susceptibility to infer that Malwa Group lavas flowed northward and concluded that the eruptive center(s) were within the Narmada Rift.”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Schöbel et al., 2014
In the citing paper
“These data along with a plagioclase 40 Ar/ 39 Ar age of 67.10 ± 0.22 Ma (Schöbel et al., 2014;recalculated to the Renne et al., 2011 calibration) suggested that the Malwa Plateau records an older history than that known in the Western Ghats where generally only Chrons 29R-29N are clearly represented.”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Schöbel et al., 2014
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Metadata
- Authors
- Schöbel, S., de Wall, H., Ganerød, M., Pandit, M. K., & Rolf, C.
- Venue
- Journal of Asian Earth Sciences
- Publisher
- Elsevier BV
- Published
- 2014-08
- Volume
- 89
- Pages
- 28-45
- ISSN
- 1367-9120
- Cited by
- 73
- References
- 0
- Language
- en
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