Carbon Fluxes and Primary Magma CO 2 Contents Along the Global Mid‐Ocean Ridge System-Reference-Cited by-同舟云学术

Carbon Fluxes and Primary Magma CO 2 Contents Along the Global Mid‐Ocean Ridge System

Published:2019-03 Issue:3 Volume:20 Page:1387-1424
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Le Voyer Marion¹²,Hauri Erik H.¹³^ORCID,Cottrell Elizabeth²^ORCID,Kelley Katherine A.⁴^ORCID,Salters Vincent J. M.⁵^ORCID,Langmuir Charles H.⁶^ORCID,Hilton David R.⁷⁸,Barry Peter H.⁹^ORCID,Füri Evelyn¹⁰^ORCID

Affiliation:

1. Department of Terrestrial Magnetism Carnegie Institution for Science Washington DC USA

2. Smithsonian Institution National Museum of Natural History Washington DC USA

3. Deceased 5 September 2018

4. Graduate School of Oceanography University of Rhode Island Narragansett RI USA

5. National High Magnetic Field Laboratory and Department of Earth, Ocean and Atmospheric Sciences Florida State University Tallahassee FL USA

6. Department of Earth and Planetary Sciences Harvard University Cambridge MA USA

7. Scripps Institution of Oceanography University of California San Diego San Diego CA USA

8. Deceased 7 January 2018

9. Department of Earth Sciences University of Oxford Oxford UK

10. Centre de Recherches Pétrographiques et Géochimiques, UMR7358, CNRS ‐ Université de Lorraine Vandoeuvre‐lès‐Nancy France

Funder

Alfred P. Sloan Foundation

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GC007630

Reference780 articles.

1. Serpentinization of abyssal peridotites from the MARK area, Mid-Atlantic Ridge: sulfur geochemistry and reaction modeling

2. The uptake of carbon during alteration of ocean crust

3. Chemical variations and regional diversity observed in MORB

4. Reconstructing CO2 concentrations in basaltic melt inclusions using Raman analysis of vapor bubbles

5. Chemical and isotopic variations along the superfast spreading East Pacific Rise from 6 to 30�S

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