APPLYING INTEGRATED GEOCHEMICAL DATA TO TRACE THE EFFECTS OF SEASONAL SNOWMELT RECHARGE IN THREE HYDROTHERMAL FLUID TYPES
DEBES II, Randall Vincent(1), FECTEAU, Kristopher(1), SANTANA, Michelle(2), LAW, Shanna L.(3), PRAPAIPONG, Panjai(1), COX, Alysia D.(3) and SHOCK, Everett L.(4)
- Abstract
- Geochemical tracers reveal sources, flow paths, and compositional changes of hot springs in Yellowstone National Park. 3 chemically distinct hot springs, sampled over 15 months, show temporal changes and snowmelt effects on differing hydrothermal fluid types.
- Presented by
- Vince Debes II
- Institution
- (1) School of Earth and Space Exploration, Arizona State University, 781 Terrace Mall, Tempe, AZ 85287; (2) Department of Education, Montana State University, 250 Reid Hall, P.O. Box 172880, Bozeman, MT 59717-2880; (3) Department of Chemistry and Geochemistry, Montana Technological University, 1300 W Park St, Butte, MT 59701; (4) School of Molecular Sciences, Arizona State University, Tempe, AZ 85287; School of Earth and Space Exploration, Arizona State University, 781 Terrace Mall, Tempe, AZ 85287
- Keywords
- Yellowstone, hydrothermal fluid, hysteresis, seasonal, hot spring