Alteration of ocean crust provides a strong temperature dependent feedback on the geological carbon cycle and is a primary driver of the Sr-isotopic composition of seawater-Reference-Cited by-同舟云学术

Alteration of ocean crust provides a strong temperature dependent feedback on the geological carbon cycle and is a primary driver of the Sr-isotopic composition of seawater

Published:2015-04 Issue: Volume:415 Page:38-46
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Coogan Laurence A.,Dosso Stan E.

Funder

NSERC

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference59 articles.

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3. The role of outcrop-to-outcrop fluid flow in off-axis oceanic hydrothermal systems under abyssal sedimentation conditions;Anderson;J. Geophys. Res.,2012

4. A hydrologic model for the uppermost oceanic crust constrained by temperature estimates from carbonate minerals;Anderson;J. Geophys. Res.,2013

5. The Phanerozoic Carbon Cycle;Berner,2004

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