Evolution of a Miocene-Pliocene Low-Angle Normal-Fault System in the Southern Bannock Range, Southeast Idaho
Geologic mapping, basin analysis, and tephrochronologic analysis in the Clifton quadrangle of southeast Idaho indicates that the modern Basin-and-Range topography is only a few million years old and that the bulk of Cenozoic extension was accommodated by slip on an older low-angle normal-fault syste...
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| Format: | Others |
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DigitalCommons@USU
2002
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| Online Access: | https://digitalcommons.usu.edu/etd/6034 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=7101&context=etd |