Spatiotemporal Evolution of Pleistocene and Late Oligocene-Early Miocene Deformation in the Mecca Hills, Southernmost San Andreas Fault Zone
Seismogenically active faults (those that produce earthquakes) are very complex systems that constantly change through time. When an earthquake occurs, the rocks surrounding a fault (the “fault rocks”) become altered or damaged. Studying these fault rocks directly can inform what processes operated...
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| Format: | Others |
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DigitalCommons@USU
2017
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| Online Access: | https://digitalcommons.usu.edu/etd/5992 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=7049&context=etd |