Stratigraphic Record of Pliocene-Pleistocene Basin Evolution and Deformation Along the San Andreas Fault, Mecca Hills, California

dc.contributor.advisorDorsey, Rebeccaen_US
dc.contributor.authorMcNabb, Jamesen_US
dc.date.accessioned2014-06-17T19:39:46Z
dc.date.available2014-06-17T19:39:46Z
dc.date.issued2014-06-17
dc.description.abstractSedimentary rocks in the Mecca Hills record a 3-4 Myr history of basin evolution and deformation within the southern San Andreas fault (SAF) zone. Detailed geologic mapping, measured sections, lithofacies analysis, and preliminary paleomagnetic data indicate that sedimentation and deformation in the Mecca Hills resulted from evolution of local fault zone complexities superimposed on regional subsidence and uplift. Sediment was derived from sources northeast of the SAF and transported southeast along the fault zone in large rivers, alluvial fans, and a smaller fault-bounded lake. Inversion of the Painted Canyon fault from oblique SW-side down to SW-side up slip was the main control on local deposition and deformation. Regional controls are suggested by an angular unconformity observed in the Mecca and Indio Hills along ~50 km of the SAF and synchronous post-740 ka uplift northeast of the SAF along ~80 km of the fault zone.en_US
dc.identifier.urihttps://hdl.handle.net/1794/17891
dc.language.isoen_USen_US
dc.publisherUniversity of Oregonen_US
dc.rightsAll Rights Reserved.en_US
dc.subjectbasin evolutionen_US
dc.subjectMecca Hillsen_US
dc.subjectpaleogeographic reconstructionen_US
dc.subjectSan Andreas faulten_US
dc.subjectstrike-slipen_US
dc.subjecttectonic reconstructionen_US
dc.titleStratigraphic Record of Pliocene-Pleistocene Basin Evolution and Deformation Along the San Andreas Fault, Mecca Hills, Californiaen_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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