Abstract
Identification by Bhattacharya et al. (1994) of seafloor spreading type magnetic anomalies in the basin lying between Laxmi Ridge in the Arabian Sea and the Indian continent necessitates a change in plate tectonic reconstruction. Naini and Talwani (1982) named this basin the Eastern Basin and we will continue to use this term in this paper. Others, in the literature, have called this the Laxmi Basin. Previous reconstructions had assumed that the Eastern Basin is underlain by continental crust. The new reconstruction moves Seychelles' original location closer to India and ameliorates a ‘space’ problem in the Mascarene Basin. A new rotation pole between anomaly 28 and 34 times avoids ‘skipping’ of fracture zones resulting from rotation poles described earlier. The negative gravity anomaly over the Eastern Basin is a necessary consequence of a continental sliver lying between oceanic crust on either side. Seismic velocities that are slightly greater than 7 km s−1 under the Eastern need not be necessarily interpreted as material that underplates continental crust.
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Talwani, M., Reif, C. Laxmi Ridge – A continental sliver in the Arabian Sea. Marine Geophysical Researches 20, 259–271 (1998). https://doi.org/10.1023/A:1004674909280
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DOI: https://doi.org/10.1023/A:1004674909280