Relation of hydraulic conductivity to depth, alteration, and rock type in the volcanic rocks of Pahute Mesa, Nevada, USA
Author:
Publisher
Springer Science and Business Media LLC
Subject
Earth and Planetary Sciences (miscellaneous),Water Science and Technology
Link
https://link.springer.com/content/pdf/10.1007/s10040-022-02571-9.pdf
Reference79 articles.
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2. Anderson SR, Kuntz MA, Davis LC (1999) Geologic controls of hydraulic conductivity in the Snake River Plain aquifer at and near the Idaho National Engineering and Environmental Laboratory, Idaho. US Geol Surv Water Resour Invest Rep 99-4033. https://doi.org/10.3133/wri994033
3. Aschwanden L, Diamond LW, Adams A (2019) Effects of progressive burial on matrix porosity and permeability of dolostones in the foreland basin of the Alpine Orogen, Switzerland. Mar Pet Geol 100:148–164. https://doi.org/10.1016/j.marpetgeo.2018.10.055
4. Bechtel Nevada (2002) A hydrostratigraphic model and alternatives for the groundwater flow and contaminant transport model of Corrective Action Units 101 and 102: central and western Pahute Mesa, Nye County, Nevada. Report DOE/NV/11718-706, US DOE. https://doi.org/10.2172/799777
5. Belcher WR, Elliott PE, Geldon AL (2001) Hydraulic-property estimates for use with a transient ground-water flow model of the Death Valley regional ground-water flow system, Nevada and California. US Geol Surv Water Resour Invest Rep 2001-4210. https://doi.org/10.3133/wri014210
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