The remelting of hydrothermally altered peridotite at mid-ocean ridges by intruding mantle diapirs

Author:

Benoit Mathieu,Ceuleneer Georges,Polvé Mireille

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Reference26 articles.

1. Dick,H. J. B., Robinson,P. T. & Meyer, P. S. The plutonic foundation of a slow-spreading ridge. American Geophysical Union monograph 70, 1–39 (1992).

2. Ross,K. & Elthon,D. Cumulates from strongly depleted mid-ocean-ridge basalt. Nature 365, 826– 829 (1993).

3. Ceuleneer,G., Monnereau,M. & Amri,I. Thermal structure of a fossil mantle diapir inferred from the distribution of mafic cumulates. Nature 379, 149–153 (1996).

4. Benoit,M., Polvé,M. & Ceuleneer, G. Trace element and isotopic characterization of mafic cumulates in a fossil mantle diapir (Oman ophiolite). Chem. Geol. 134, 199–214 ( 1996).

5. Grove,T. L., Kinzler,R. J. & Bryan, W. B. in Mantle Flow and Melt Generation at Mid-ocean Ridges (eds Phipps Morgan, J., Blackman, D. K. & Sinton, J. M.) 281–310 (AGU Geophysical Monographs, 71, 1992).

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