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U.S. Department of Energy
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Preliminary report on late Cenozoic faulting and stratigraphy in the vicinity of Yucca Mountain, Nye County, Nevada

Technical Report ·
OSTI ID:59683

Mapping of surficial deposits and examination of faults in natural and trenched exposures in a 1100 km{sup 2} area around the site of a potential repository for radioactive waste at Yucca Mountain have identified 32 faults that offset or fracture Quaternary deposits. Where the amount of Quarternary offset can be estimated, dip-slip movement is on the order of 3 m or less on faults in and near Yucca Mountain. Maximum Quarternary offset within the study area may be as much as 30 m. No strike-slip movement was demonstrated nor can it be ruled out. Based on radiometric ages, correlations of stratigraphic units, and field observations, Quarternary faults are divided into three broad age groups: five faults moved between about 270,000 and 40,000 years ago; four faults moved about 1 m.y. ago and 23 faults moved probably between 2 m.y. and more than 1.2 m.y. ago. Offset of Holocene deposits has not been demonstrated.

Research Organization:
Geological Survey, Denver, CO (United States)
DOE Contract Number:
AI08-78ET44802
OSTI ID:
59683
Report Number(s):
USGS-OFR--84-788; ON: DE85007591
Country of Publication:
United States
Language:
English