Data Synthesis: Multicomponent Mapping of the Sulfur Springs Geothermal Area, Valles Caldera, New Mexico, Combining Geologic, Structural, and Geochemical Data
The Valles Caldera in the Jemez Mountains, New Mexico exhibits modern hydrothermal and fumarolic activity. The ~22-km-diameter caldera was formed by two large eruptions (>300 km3) at 1.6 Ma and 1.2 Ma. The caldera-forming eruptions were followed by re-fill of the magma chamber that resulted in a resurgent dome, a long period of lava dome formation (~1.2 Ma to ~0.5 Ma), and a series of explosive and effusive events in the SW sector of the caldera, the youngest of which occurred between ~70 ka and ~40 ka. Today, the Valles caldera has a well-developed hydrothermal system. Many locations within the caldera host warm springs and fumaroles. The most notable of these sites is Sulfur Springs in the western portion of the resurgent dome. Past mapping efforts of the Sulfur Springs area have not been integrated with investigations documenting the gas and spring chemistry. Thus, it is not well known how the locations of hydrothermal features are related to the shallow geology and structural features. Furthermore, the interactions between the different hydrothermal fluids have not been well characterized. To address these questions, I have created a multi-parameter map of the Sulfur Springs area (1:2500 scale) that includes structural and geothermal features overlain by water chemistry and CO2 gas concentration. I show that surface geothermal features are related to fault locations and suggest that magmatic gasses use the faults as pathways to reach the surface. I also show that magmatic gas dissolution produces highly acidic water (pH <2) and propose a conceptual model for a subsurface storage zone which allows for mixing of these fluids. Measured gas concentrations in one hot spring (~2 meters in diameter) at 4 separate degassing sites show different temporal patterns and a large range in CO2 concentration (302-10545 ppm). Such fine scale variation in concentration and temporal pattern is not widely documented in similar systems. Thus, I propose future studies into temporal gas measurements of caldera-hosted hydrothermal systems incorporate fine scale measurements to discern if this is a phenomenon common amongst these systems.
Details
- Kramer, Jacob Levi (Author)
- Clarke, Amanda (Thesis advisor)
- Hartnett, Hilairy (Thesis advisor)
- Arrowsmith, Ramon (Committee member)
- Arizona State University (Publisher)
- en
- Partial requirement for: M.S., Arizona State University, 2024
- Field of study: Geological Sciences
Additional Information
- 81 pages