Indian Ocean floor deformation induced by the Reunion plume rather than the Tibetan Plateau
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/s41561-018-0110-z.pdf
Reference55 articles.
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2. Bull, J. M. & Scrutton, R. A. Seismic reflection images of intraplate deformation, central Indian Ocean, and their tectonic significance. J. Geol. Soc. Lond. 149, 955–966 (1992).
3. Krishna, K. S. et al. Periodic deformation of oceanic crust in the central Indian Ocean. J. Geophys. Res. 103, 17859–17875 (1998).
4. Curray, J. R., Emmel, F. J. & Moore, D. G. The Bengal Fan: morphology, geometry, stratigraphy, history and processes. Mar. Pet. Geol. 19, 1191–1223 (2002).
5. Wiens, D. A. et al. A diffuse plate boundary model for Indian Ocean tectonics. Geophys. Res. Lett. 12, 429–432 (1985).
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