Fault-controlled hydration of the upper mantle during continental rifting-Reference-Cited by-同舟云学术

Fault-controlled hydration of the upper mantle during continental rifting

Published:2016-03-07 Issue:5 Volume:9 Page:384-388
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Bayrakci G.,Minshull T. A.,Sawyer D. S.,Reston T. J.,Klaeschen D.,Papenberg C.,Ranero C.,Bull J. M.,Davy R. G.,Shillington D. J.,Perez-Gussinye M.,Morgan J. K.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo2671.pdf

Reference34 articles.

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2. Whitmarsh, R. B., Manatschal, G. & Minshull, T. A. Evolution of magma-poor continental margins from rifting to seafloor spreading. Nature 413, 150–154 (2001).

3. Perez-Gussinye, M. & Reston, T. J. Rheological evolution during extension at nonvolcanic rifted margins: onset of serpentinization and development of detachments leading to continental breakup. J. Geophys. Res. 106, 3961–3975 (2001).

4. Ranero, C. R. et al. Bending-related faulting and mantle serpentinization at the Middle America trench. Nature 425, 367–373 (2003).

5. Manning, C. E. & Ingebritsen, S. E. Permeability of the continental crust: implications of geothermal data and metamorphic systems. Rev. Geophys. 37, 127–150 (1999).

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