Abstract
[Muller et al. (2013)][1] present an interesting hypothesis that quantifies a relationship between temporal changes in the ratio of Mg and Ca in seawater and global hydrothermal flux through oceanic crust. The relationship is quantified through estimates of the area of oceanic crust <65 m.y. old
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
