author_facet Bennett, R. A.
Wernicke, B. P.
Davis, J. L.
Elósegui, P.
Snow, J. K.
Abolins, M. J.
House, M. A.
Stirewalt, G. L.
Ferrill, D. A.
Bennett, R. A.
Wernicke, B. P.
Davis, J. L.
Elósegui, P.
Snow, J. K.
Abolins, M. J.
House, M. A.
Stirewalt, G. L.
Ferrill, D. A.
author Bennett, R. A.
Wernicke, B. P.
Davis, J. L.
Elósegui, P.
Snow, J. K.
Abolins, M. J.
House, M. A.
Stirewalt, G. L.
Ferrill, D. A.
spellingShingle Bennett, R. A.
Wernicke, B. P.
Davis, J. L.
Elósegui, P.
Snow, J. K.
Abolins, M. J.
House, M. A.
Stirewalt, G. L.
Ferrill, D. A.
Geophysical Research Letters
Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
General Earth and Planetary Sciences
Geophysics
author_sort bennett, r. a.
spelling Bennett, R. A. Wernicke, B. P. Davis, J. L. Elósegui, P. Snow, J. K. Abolins, M. J. House, M. A. Stirewalt, G. L. Ferrill, D. A. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/97gl02951 <jats:p>We estimated horizontal velocities at 15 locations in the vicinity of Yucca Mountain, Nevada, from Global Positioning System surveys conducted between 1991 and 1996. We used these velocity estimates to infer slip rates on two major Quaternary faults within the eastern California shear zone (ECSZ), the Hunter Mountain and Death Valley faults. The sum of slip rates across the two faults is well determined at 5 ± 1 mm/yr (1‐σ). Between 3 to 5 mm/yr of this motion appears to be accommodated along the Death Valley fault, implying 30–50 m of strain accumulation over the next 10,000 yr. If so, there is potential for 5 to 10 M<jats:italic><jats:sub>w</jats:sub></jats:italic> 6.5–7.5 earthquakes during this period, a finding consistent with paleoseismological studies of the fault zone. Yucca Mountain, which lies 50 km east of the ECSZ, is the proposed location for the disposal of high‐level nuclear waste in the United States.</jats:p> Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada Geophysical Research Letters
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series Geophysical Research Letters
source_id 49
title Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_unstemmed Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_full Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_fullStr Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_full_unstemmed Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_short Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_sort global positioning system constraints on fault slip rates in the death valley region, california and nevada
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1029/97gl02951
publishDate 1997
physical 3073-3076
description <jats:p>We estimated horizontal velocities at 15 locations in the vicinity of Yucca Mountain, Nevada, from Global Positioning System surveys conducted between 1991 and 1996. We used these velocity estimates to infer slip rates on two major Quaternary faults within the eastern California shear zone (ECSZ), the Hunter Mountain and Death Valley faults. The sum of slip rates across the two faults is well determined at 5 ± 1 mm/yr (1‐σ). Between 3 to 5 mm/yr of this motion appears to be accommodated along the Death Valley fault, implying 30–50 m of strain accumulation over the next 10,000 yr. If so, there is potential for 5 to 10 M<jats:italic><jats:sub>w</jats:sub></jats:italic> 6.5–7.5 earthquakes during this period, a finding consistent with paleoseismological studies of the fault zone. Yucca Mountain, which lies 50 km east of the ECSZ, is the proposed location for the disposal of high‐level nuclear waste in the United States.</jats:p>
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author Bennett, R. A., Wernicke, B. P., Davis, J. L., Elósegui, P., Snow, J. K., Abolins, M. J., House, M. A., Stirewalt, G. L., Ferrill, D. A.
author_facet Bennett, R. A., Wernicke, B. P., Davis, J. L., Elósegui, P., Snow, J. K., Abolins, M. J., House, M. A., Stirewalt, G. L., Ferrill, D. A., Bennett, R. A., Wernicke, B. P., Davis, J. L., Elósegui, P., Snow, J. K., Abolins, M. J., House, M. A., Stirewalt, G. L., Ferrill, D. A.
author_sort bennett, r. a.
container_issue 23
container_start_page 3073
container_title Geophysical Research Letters
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description <jats:p>We estimated horizontal velocities at 15 locations in the vicinity of Yucca Mountain, Nevada, from Global Positioning System surveys conducted between 1991 and 1996. We used these velocity estimates to infer slip rates on two major Quaternary faults within the eastern California shear zone (ECSZ), the Hunter Mountain and Death Valley faults. The sum of slip rates across the two faults is well determined at 5 ± 1 mm/yr (1‐σ). Between 3 to 5 mm/yr of this motion appears to be accommodated along the Death Valley fault, implying 30–50 m of strain accumulation over the next 10,000 yr. If so, there is potential for 5 to 10 M<jats:italic><jats:sub>w</jats:sub></jats:italic> 6.5–7.5 earthquakes during this period, a finding consistent with paleoseismological studies of the fault zone. Yucca Mountain, which lies 50 km east of the ECSZ, is the proposed location for the disposal of high‐level nuclear waste in the United States.</jats:p>
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spelling Bennett, R. A. Wernicke, B. P. Davis, J. L. Elósegui, P. Snow, J. K. Abolins, M. J. House, M. A. Stirewalt, G. L. Ferrill, D. A. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/97gl02951 <jats:p>We estimated horizontal velocities at 15 locations in the vicinity of Yucca Mountain, Nevada, from Global Positioning System surveys conducted between 1991 and 1996. We used these velocity estimates to infer slip rates on two major Quaternary faults within the eastern California shear zone (ECSZ), the Hunter Mountain and Death Valley faults. The sum of slip rates across the two faults is well determined at 5 ± 1 mm/yr (1‐σ). Between 3 to 5 mm/yr of this motion appears to be accommodated along the Death Valley fault, implying 30–50 m of strain accumulation over the next 10,000 yr. If so, there is potential for 5 to 10 M<jats:italic><jats:sub>w</jats:sub></jats:italic> 6.5–7.5 earthquakes during this period, a finding consistent with paleoseismological studies of the fault zone. Yucca Mountain, which lies 50 km east of the ECSZ, is the proposed location for the disposal of high‐level nuclear waste in the United States.</jats:p> Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada Geophysical Research Letters
spellingShingle Bennett, R. A., Wernicke, B. P., Davis, J. L., Elósegui, P., Snow, J. K., Abolins, M. J., House, M. A., Stirewalt, G. L., Ferrill, D. A., Geophysical Research Letters, Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada, General Earth and Planetary Sciences, Geophysics
title Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_full Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_fullStr Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_full_unstemmed Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_short Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
title_sort global positioning system constraints on fault slip rates in the death valley region, california and nevada
title_unstemmed Global Positioning System constraints on fault slip rates in the Death Valley Region, California and Nevada
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1029/97gl02951