The origin and fate of C during alteration of the oceanic crust

Author:

Martinez Isabelle,Shilobreeva Svetlana,Alt Jeffrey,Polyakov Veniamin,Agrinier Pierre

Publisher

Cellule MathDoc/CEDRAM

Subject

General Earth and Planetary Sciences,Global and Planetary Change

Reference63 articles.

1. O and H stable isotope compositions of oceanic crust and upper mantle rocks exposed in the Hess Deep near the Galapagos Triple Junction;['Agrinier, P.', 'Hekinian, R.', 'Bideau, D.', 'Javoy, M.'];Earth Planet. Sci. Lett.,1995a

2. Stable isotope ratios (oxygen, hydrogen) and petrology of hydrothermally altered dolerites at the bottom of the sheeted dike complex of Hole 504B;['Agrinier, P.', 'Laverne, C.', 'Tartarotti, P.', 'Erzinger, J.', 'Becker, K.', 'Dick, H. J. B.', 'Stokking, L. B.'];Proceedings of the Ocean Drilling Program - Scientific Results,1995b

3. Microbial sulfate reduction and the sulfur budget for a complete section of altered oceanic basalts, IODP Hole 1256D (eastern Pacific);['Alt, J. C.', 'Shanks, W. C.'];Earth Planet. Sci. Lett.,2011

4. The uptake of carbon during alteration of ocean crust;['Alt, J. C.', 'Teagle, D. A. H.'];Geochim. Cosmochim. Acta,1999

5. Hydrothermal alteration of upper oceanic crust formed at fast-spreading ridge: mineral, chemical, and isotopic evidence from ODP Site 801;['Alt, J. C.', 'Teagle, D. A. H.'];Chem. Geol.,2003

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