Subseafloor Fluid and Chemical Fluxes Along a Buried‐Basement Ridge on the Eastern Flank of the Juan de Fuca Ridge
Author:
Affiliation:
1. Moss Landing Marine Laboratories Moss Landing CA USA
2. College of Fisheries and Ocean SciencesUniversity of Alaska Fairbanks Fairbanks AK USA
Funder
National Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008408
Reference74 articles.
1. Iron and sulfide oxidation within the basaltic ocean crust: implications for chemolithoautotrophic microbial biomass production
2. A geological and geophysical investigation of Baby Bare, locus of a ridge flank hydrothermal system in the Cascadia Basin
3. Behavior of Li, Rb and Cs during basalt glass and olivine dissolution and chlorite, smectite and zeolite precipitation from seawater: Experimental investigations and modelization between 50° and 300°C
4. The effect of low-temperature alteration of basalt on the oceanic budget of potassium
5. Fluid–sediment interactions related to hydrothermal circulation in the Eastern Flank of the Juan de Fuca Ridge
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