HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Similar articles in ISI Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Dinwiddie, C. L. Articles by Ferrill, D. A. Search for Related Content PubMed Articles by Dinwiddie, C. L. Articles by Ferrill, D. A. GeoRef GeoRef Citation Agricola Articles by Dinwiddie, C. L. Articles by Ferrill, D. A. Related Collections Capillary Barriers Field-Scale Studies Spatial Variability Fractured Rock

ORIGINAL RESEARCH

Fault Zone Deformation Overprints Permeability of Nonwelded Ignimbrite: Chalk Cove Fault, Bishop Tuff, Bishop, California

^a Center for Nuclear Waste Regulatory Analyses, Geosciences and Engineering Division of Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238
^b Utah Faults, Fractures, and Fluids (UF³), Innovation Campus, Utah State Univ., 1770 Research Park Way, Ste. 183, North Logan, UT 84341
^c now at Dept. of Earth, Material, and Planetary Sciences, Geosciences and Engineering Division of Southwest Research Institute
^d now at U.S. Nuclear Regulatory Commission
^* Corresponding author (cdinwiddie{at}swri.org)

Received 2 May 2005.

Deformation-induced secondary heterogeneities associated with a steeply-dipping normal fault in the nonwelded Bishop Tuff were examined in a multidisciplinary study using in situ gas permeability tests, structural mapping, and laboratory analyses as analogs for fault deformation features within the poorly exposed Paintbrush nonwelded hydrogeologic unit at Yucca Mountain, Nevada. Three features of fault-zone deformation were identified that may act to constrain lateral flow in unsaturated nonwelded ignimbrites. First, development of a fault gouge, with a decrease in grain size caused by grain comminution, decreases the permeability of this element with respect to the host rock. Second, long open fractures paralleling the fault have an increased permeability with respect to the host rock. Third, small-scale fractures and grain rotation in adjacent matrix blocks induce an interconnected porosity not seen in host rock. Intrinsic permeability variation beyond what is observed in the host rock reflects the effect of small-scale deformation in the matrix adjacent the fault. These features can reduce the continuity of potential capillary or permeability barriers, and thus limit any redistribution of percolation that would result from lateral flow diversion.

Abbreviations: PTn, Paintbrush nonwelded [unit] • TCw, Tiva Canyon welded [unit] • TSw, Topopah Spring welded [unit] • XRD, X-ray diffraction