Can high-temperature, high-heat flux hydrothermal vent fields be explained by thermal convection in the lower crust along fast-spreading Mid-Ocean Ridges?-Reference-Cited by-同舟云学术

Can high-temperature, high-heat flux hydrothermal vent fields be explained by thermal convection in the lower crust along fast-spreading Mid-Ocean Ridges?

Published:2017-05 Issue:5 Volume:18 Page:1907-1925
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Fontaine Fabrice J.¹²,Rabinowicz M.³,Cannat M.¹^ORCID

Affiliation:

1. Institut de Physique du Globe de Paris, UMR CNRS 7154; Paris France

2. Now at Observatoire du Piton de la Fournaise, La Réunion Island

3. Laboratoire GET, UMR CNRS 5563; Toulouse France

Funder

French INSU-Syster program

IPGP

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006737/fullpdf

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