Accretion mode of oceanic ridges governed by axial mechanical strength-Reference-Cited by-同舟云学术

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Accretion mode of oceanic ridges governed by axial mechanical strength

Published:2018-03-26 Issue:4 Volume:11 Page:274-279
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Sibrant A. L. R.,Mittelstaedt E.,Davaille A.,Pauchard L.,Aubertin A.,Auffray L.,Pidoux R.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/s41561-018-0084-x.pdf

Reference64 articles.

1. Schouten, H., Klitgord, K. D. & Whitehead, J. A. Segmentation of mid-ocean ridges. Nature 317, 225–229 (1985).

2. MacDonald, K. C. et al. A new view of the mid-ocean ridge from the behavior of ridge-axis discontinuities. Nature 335, 217–225 (1988).

3. Lin, J. & Parmentier, E. M. A finite amplitude necking model of rifting in brittle lithosphere. J. Geophys. Res. 95, 4909–4923 (1990).

4. Phipps Morgan, J. & Chen, J. Dependence of ridge-axis morphology on magma supply and spreading rate. Nature 364, 706–708 (1993).

5. Oldenburg, D. W. & Brune, J. N. An explanation for the orthogonality of ocean ridges and transform faults. J. Geophys. Res. 80, 2575–2585 (1975).

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