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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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North America
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Basin and Range Province (3)
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North American Cordillera (1)
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U. S. Rocky Mountains
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North America
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Basin and Range Province (3)
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North American Cordillera (1)
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Rocky Mountains
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U. S. Rocky Mountains
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Wasatch Range (1)
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Western Interior (1)
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Western Overthrust Belt (1)
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United States
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Colorado Plateau (1)
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Utah
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Beaver County Utah
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Roosevelt Hot Springs KGRA (1)
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Davis County Utah (1)
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Salt Lake County Utah
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Wasatch fault zone (2)
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Extensional Tectonics of Eastern Basin-Range/Overthrust Belt: Inferences on Structural Style from Reflection Data, Surface Geology, and Rheologic Models: ABSTRACT
Preface to seismicity of the Wasatch Front and Great Basin-Sierra Nevada boundary
Earthquake studies along the Wasatch front, Utah: Network monitoring, seismicity, and seismic hazards
Slip vectors on faults near Salt Lake City, Utah, from quaternary displacements and seismicity
Temporal monitoring of seismic velocity along the Wasatch Front using quarry blasts
A summary of the geology, geochemistry, and geophysics of the Roosevelt hot springs thermal area, Utah
The possibility of relating seismicity to Cenozoic tectonics in the Western United States has led to the need for a compilation and a map of fault-plane solutions for this area. For several years the U.S. Geological Survey has determined fault-plane solutions from their seismograph arrays, principally in California and Nevada. These data were summarized by Lindh and others (1973). Fault-plane solutions for the Intermountain region, including Utah, Idaho, Nevada, Montana, and Wyoming, were compiled by Smith and Sbar (1974). Following these compilations, many new fault-plane solutions were published as the result of detailed analyses of earthquakes recorded by portable and new permanent seismograph arrays. Our intent here is to provide a tabulation (Table 5-1, in pocket) and map of the principal fault-plane solutions (Fig. 5-1, P1. 5-1, in pocket) for the Western United States through 1975 and part of 1976. For each fault-plane solution, the tabulations list the type of solution (single event, S; composite, C), date, time (GMT), location, attitudes of P - and T -axes, nodal-plane attitudes, and the reference. Because of the wide variety of types and sizes of seismograph arrays and the differences in data analyses, we have not attempted to analyze the quality of individual solutions; however, we have differentiated between single-event solutions (large symbols) and composite solutions (small symbols) on the map (Fig. 5-1). Generally, a single-event solution was determined from an earthquake of magnitude ( M ) 5.0 or larger, unless it was recorded within a dense array such as in the U.S. Geological Survey Nevada test-site