The Amirante Ridge and Trench System in the Indian Ocean: the southern termination of the NW Indian subduction

Author:

Rodriguez Mathieu

Publisher

Cellule MathDoc/CEDRAM

Subject

General Earth and Planetary Sciences,Global and Planetary Change

Reference82 articles.

1. [Agard et al., 2018] Agard, P.; Plunder, A.; Angiboust, S.; Bonnet, G.; Ruh, J. The subduction plate interface: rock record and mechanical coupling (from long to short timescales), Lithos, Volume 320–321 (2018), pp. 537-566

2. [Ali and Aitchison, 2008] Ali, J. R.; Aitchison, J. C. Gondwana to Asia: Plate tectonics, paleogeography and the biological connectivity of the Indian sub-continent from the Middle Jurassic through latest Eocene (166–35 Ma), Earth-Sci. Rev., Volume 88 (2008), pp. 145-166

3. [Beck et al., 1995] Beck, R. A.; Burbank, D. W.; Sercombe, W. J.; Riley, G. W.; Barndt, J. K.; Berry, J. R.; Afzal, J.; Khan, A. M.; Jurgen, H.; Metje, J.; Cheema, A.; Shafique, N. A.; Lawrence, R. D.; Khan, A. Stratigraphic evidence for an early collision between northwest India and Asia, Nature, Volume 373 (1995), pp. 55-58

4. [Bernard and Munschy, 2000] Bernard, A.; Munschy, M. Le bassin des Mascareignes et le bassin de Laxmi (océan Indien occidental) se sont-ils formés à l’axe d’un même centre d’expansion?, C. R. Acad. Sci. Paris, Volume 330 (2000), pp. 777-783

5. [Besse and Courtillot, 1988] Besse, J.; Courtillot, V. Paleogeographic maps of the continents bordering the Indian Ocean since the Early Jurassic, J. Geophys. Res., Volume 93 (1988), pp. 11791-11808

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