The importance of talc and chlorite “hybrid” rocks for volatile recycling through subduction zones; evidence from the high-pressure subduction mélange of New Caledonia

Author:

Spandler Carl,Hermann Jörg,Faure Kevin,Mavrogenes John A.,Arculus Richard J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference109 articles.

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2. Ague JJ (2006) Models of permeability contrasts in subduction zone mélange: implications for gradients in fluid fluxes, Syros and Tinos Islands, Greece. Chem Geol (in press)

3. Bach W, Garrido CJ, Paulick H, Harvey J, Rosner M (2004) Seawater-peridotite interactions: first insights from ODP Leg 209, MAR 15°N. Geochem Geophys Geosyst 5:Q09F26

4. Barnicoat AC, Cartwright I (1995) Focused fluid flow during subduction: oxygen isotope data from high-pressure ophiolites of the western Alps. Earth Planet Sci Lett 132:53–61

5. Bau M, Dulski P, Möller P (1995) Yttrium and Holmium in South Pacific seawater: vertical distribution and possible fractionation mechanisms. Chem Erde Geochem 55:1–15

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