Peter P. Scheuermann scite author profile

Highlights:1. MOR vent fluids show the largest range of δ 138/134 Ba seen so far in marine systems.2. Endmember vent fluid δ 138/134 Ba values are the same as those of the source rocks.3. Barite precipitation leads to high δ 138/134 Ba values in vent fluids as they evolve.4. Hydrothermal Ba input may explain non-conservative δ 138/134 Ba seen in deep waters.5. Hydrothermal input contributes 3-9% of the Ba in some Atlantic deep waters.

show abstract

Geochemical heterogeneity of sublacustrine hydrothermal vents in Yellowstone Lake, Wyoming

Fowler

Tan

Luttrell

et al. 2019

Journal of Volcanology and Geothermal Research

View full text Add to dashboard Cite

scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.

Contact Info

hi@scite.ai

10624 S. Eastern Ave., Ste. A-614

Henderson, NV 89052, USA

Blog Terms and Conditions API Terms Privacy Policy Contact Cookie Preferences Do Not Sell or Share My Personal Information

Made with 💙 for researchers

Part of the Research Solutions Family.

Peter P. Scheuermann

Vapor-driven sublacustrine vents in Yellowstone Lake, Wyoming, USA

Predicting the potential for mineral scale precipitation in unconventional reservoirs due to fluid-rock and fluid mixing geochemical reactions

Barium isotopes in mid-ocean ridge hydrothermal vent fluids: A source of isotopically heavy Ba to the ocean

Geochemical heterogeneity of sublacustrine hydrothermal vents in Yellowstone Lake, Wyoming

Contact Info

Product

Resources

About