Abstract
Continuous fluxing at a decreasing rate of mantle Cl and Br by volcanism throughout the Earth's history can account for the mass of Cl and Br, and the Cl/Br ratio, of the oceans. © 1978 Nature Publishing Group.
Cite
CITATION STYLE
APA
Schilling, J. G., Unni, C. K., & Bender, M. L. (1978). Origin of chlorine and bromine in the oceans. Nature, 273(5664), 631–636. https://doi.org/10.1038/273631a0
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free