Magmatic volatiles in the Yellowstone Plateau volcanic field: The knowns, the unknowns, and the uncertainties
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Abstract
The Yellowstone Plateau volcanic field has a large magmatic system supplying heat and mass into the overlying hydrothermal system. To interpret changes in the composition and/or emission rates of hydrothermal fluids as possible indicators of volcanic unrest requires discriminating between magmatic, crustal, hydrothermal, and hybrid sources and processes. Significant progress in characterizing the composition and rates of hydrothermal fluid discharge has been made over the past two decades but many uncertainties about sources and processes remain.
Study Area
| Publication type | Conference Paper |
|---|---|
| Publication Subtype | Conference Paper |
| Title | Magmatic volatiles in the Yellowstone Plateau volcanic field: The knowns, the unknowns, and the uncertainties |
| DOI | 10.13125/unicapress.978-88-3312-187-1 |
| Publication Date | May 29, 2025 |
| Year Published | 2025 |
| Language | English |
| Publisher | UNICApress |
| Contributing office(s) | Volcano Science Center |
| Description | 4 p. |
| Larger Work Type | Book |
| Larger Work Subtype | Conference publication |
| Larger Work Title | Proceedings of the 3rd IAGC international conference: Water rock interaction-18 & applied isotope geochemistry-15 |
| First page | 78 |
| Last page | 81 |
| Country | United States |
| State | Wyoming |
| Other Geospatial | Yellowstone Plateau volcanic field |