The Systematics of Stable Hydrogen (δ2H) and Oxygen (δ18O) Isotopes and Tritium (3H) in the Hydrothermal System of the Yellowstone Plateau Volcanic Field, USA

Abstract To improve our understanding of hydrothermal activity on the Yellowstone Plateau volcanic field, we collected and analyzed a large data set of δ2H, δ18O, and the 3H concentrations of circum‐neutral and alkaline waters. We find that (a) hot springs are fed by recharge throughout the volcanic...

Olles dieđut

Bibliográfalaš dieđut

Váldodahkkit:	Shaul Hurwitz, R. Blaine McCleskey, Bryant C. Jurgens, Jacob B. Lowenstern, Laura Clor, Andrew G. Hunt
Materiálatiipa:	Artigo
Giella:	Inglês
Almmustuhtton:	Wiley 2025-07-01
Ráidu:	Geochemistry, Geophysics, Geosystems
Fáttát:	water‐rock interaction meteoric water hot spring groundwater stable isotopes rhyolite
Liŋkkat:	https://doi.org/10.1029/2025GC012230
Fáddágilkorat:	Lasit fáddágilkoriid Eai fáddágilkorat, Lasit vuosttaš fáddágilkora!