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Paleomagnetism and tectonics of a Deccan trap lava sequence at Amarkantak, India
Abstract
Detailed paleomagnetic measurements have been made on a lava sequence exposed between altitudes of 700 to 1000 meters in the Amarkantak-Dindori tract on the eastern margin of the Deccan traps. The variation in the direction of remanent magnetism with altitude has been studied. The paleomagnetic data reveal the occurrence of a reversal of the earth's magnetic field at an altitude of about 975 meters at Amarkantak as well as the unstable behavior of the geomagnetic field near the polarity transition. These data are at variance with the observation of the same reversal of magnetic field at an altitude of about 625 meters in the paleomagnetic study of several other vertical sequences in the Deccan traps. The variance is interpreted in terms of an uplift of the Amarkantak region by about 350 meters.
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“available data suggests that the Mandla subprovince hosted not only the early magmatics and some of the oldest Deccan CFB”
From Spatio-temporal volume recalibration shows Deccan volcanism caused Terminal Cretaceous Mass Extinction (2026) · cites this paper as Athavale, 1970
Citations
Cites
No references could be resolved yet.
Research works printed but not linked: 14
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- Sahasrabudhe, 1963, Palaeomagnetism and the Geology of the Deccan Traps: Seminar on Geophysical Investigations in the Peninsular Shield, 226
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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
Metadata
- Authors
- Athavale, R. N.
- Venue
- Journal of Geophysical Research
- Publisher
- American Geophysical Union (AGU)
- Published
- 1970-07-10
- Volume
- 75
- Issue
- 20
- Pages
- 4000-4006
- ISSN
- 0148-0227
- Cited by
- 32
- References
- 0
- Language
- en
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- Athavale, R. N. (1970). Paleomagnetism and tectonics of a Deccan trap lava sequence at Amarkantak, India. Journal of Geophysical Research. https://doi.org/10.1029/jb075i020p04000