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
L. A. CooganSchool of Earth and Ocean Sciences, University of Victoria, Victoria, BC, CanadaStan E. DossoSchool of Earth and Ocean Sciences, University of Victoria, Victoria, BC, Canada
2015en
ABI
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Cited by 20 references