Michael F. Fahy scite author profile

This hydraulic connection across geologic and lithostratigraphic contacts is believed to result from interconnected faults, fractures, and intervals with large matrix permeability. Samples of UE-25 c #3 water, analyzed from 1995 to 1997, seem to indicate that changes in the quality of the water pumped from that well are probably due solely to lateral variations in water quality within the tuffaceous rocks.

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Michael F. Fahy

Analysis of a multiple-well interference test in Miocene tuffaceous rocks at the C-Hole complex, May--June 1995, Yucca Mountain, Nye County, Nevada

Dual-porosity analysis of conservative tracer testing in saturated volcanic rocks at Yucca Mountain in NYE County, Nevada

Deformation Targeting for Fractured Reservoirs: ABSTRACT

Results from geothermal logging, air and core-water chemistry sampling, air-injection testing, and tracer testing in the northern Ghost Dance Fault, Yucca Mountain, Nevada, November 1996 to August 1998

Results of Hydraulic Tests in Miocene Tuffaceous Rocks at the C-Hole Complex, 1995 to 1997, Yucca Mountain, Nye County, Nevada

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