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Self-Organizing Fluid Flow Patterns In Crystalline Rock: Theoretical Approach To The Hydrothermal Systems In The Middle Fork Of The Boise River, Scott A. Himes
Self-Organizing Fluid Flow Patterns In Crystalline Rock: Theoretical Approach To The Hydrothermal Systems In The Middle Fork Of The Boise River, Scott A. Himes
Theses and Dissertations
The thermal springs along the Middle Fork of the Boise River (MFBR) within the Atlanta lobe of the Idaho batholith discharge in discrete locations that appear to be part of self-organizing flow systems. Infiltrating water flows through Basin and Range fractures to depth where it is heated and ultimately discharged at the intersection of trans-Challis oriented faults along the MFBR. Isotopic compositions of the thermal waters have a linear trend with elevation suggesting that the recharge locations are near each thermal spring and the hydrothermal system is not one large interconnected system, but rather multiple individual hydrothermal systems. Water chemically …