Continuous exhumation of mantle-derived rocks at the Southwest Indian Ridge for 11 million years-Reference-Cited by-同舟云学术

Continuous exhumation of mantle-derived rocks at the Southwest Indian Ridge for 11 million years

Published:2013-03-24 Issue:4 Volume:6 Page:314-320
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Sauter Daniel,Cannat Mathilde,Rouméjon Stéphane,Andreani Muriel,Birot Dominique,Bronner Adrien,Brunelli Daniele,Carlut Julie,Delacour Adélie,Guyader Vivien,MacLeod Christopher J.,Manatschal Gianreto,Mendel Véronique,Ménez Bénédicte,Pasini Valerio,Ruellan Etienne,Searle Roger

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo1771.pdf

Reference48 articles.

1. Dick, H. J. B., Lin, J. & Schouten, H. An ultraslow-spreading class of ocean ridge. Nature 426, 405–412 (2003).

2. Sauter, D. & Cannat, M. in Diversity of Hydrothermal Systems on Slow-Spreading Ocean Ridges (eds Peter, R., Colin, D., Jérome, D. & Bramley, M.) 153–173 (Geophysical Monograph Series, Vol. 188, AGU, 2010).

3. Patriat, P., Sloan, H. & Sauter, D. From slow to ultra-slow: A previously undetected event at the Southwest Indian Ridge at ∼ 24 Myr. Geology 36, 207–210 (2008).

4. Cannat, M. et al. Spreading rate, spreading obliquity, and melt supply at the ultraslow spreading Southwest Indian Ridge. Geochem. Geophys. Geosyst. 9, Q04002 (2008).

5. Cannat, M., Rommevaux-Jestin, C., Sauter, D., Deplus, C. & Mendel, V. Formation of the axial relief at the very slow spreading Southwest Indian Ridge (49°–69° E). J. Geophys. Res. 104, 22825–22843 (1999).

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