Structural Evolution of the Virgin Spring Phase of the Amargosa Chaos, Death Valley, California, USA

dc.contributor.advisorMiller, Marlien_US
dc.contributor.authorCastonguay, Samuelen_US
dc.date.accessioned2013-10-10T23:18:57Z
dc.date.available2013-10-10T23:18:57Z
dc.date.issued2013-10-10
dc.description.abstractThe Amargosa Chaos and Fault of Death Valley are complex features that play important roles in various tectonic models. Some recent models claim the fault is a regional detachment accommodating 80 km of NW-directed transport that produced the Chaos in its hangingwall. I offer an alternative interpretation: the chaos is a product of multiphase deformation that likely spanned the late Mesozoic and Cenozoic. The Amargosa Fault represents just one of six deformation events. The accompanying map (supplemental file) shows the cross-cutting relationships among fault populations: (D1) 25% north-northwest directed shortening across an imbricate thrust and tight fold system; (D2) E-SE extension on five normal faults; (D3) extension-related folding, which folded the D2 faults; (D4) normal-oblique slip on the Amargosa Fault; (D5) E-W extension on domino faults; (D6) extension on the Black Mountains Frontal Fault. The D2 faults, not the Amargosa, created the enigmatic attenuation observed in the Chaos.en_US
dc.identifier.urihttps://hdl.handle.net/1794/13418
dc.language.isoen_USen_US
dc.publisherUniversity of Oregonen_US
dc.rightsAll Rights Reserved.en_US
dc.subjectAmargosa Chaosen_US
dc.subjectDeath Valleyen_US
dc.subjectStructural Geologyen_US
dc.titleStructural Evolution of the Virgin Spring Phase of the Amargosa Chaos, Death Valley, California, USAen_US
dc.typeElectronic Thesis or Dissertationen_US
thesis.degree.disciplineDepartment of Geological Sciencesen_US
thesis.degree.grantorUniversity of Oregonen_US
thesis.degree.levelmastersen_US
thesis.degree.nameM.S.en_US

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