Generation of Structural Relief by Fault Propagation Folding, Tien Shan, Kyrgzstan

dc.contributor.advisorHopkins, Samanthaen_US
dc.contributor.authorPaulson, Kathrynen_US
dc.date.accessioned2013-10-10T23:19:25Z
dc.date.available2013-10-10T23:19:25Z
dc.date.issued2013-10-10
dc.description.abstractThe southern margin of the Kochkor Basin in the Kyrgyz Tien Shan is actively shortening. The South Kochkor Fault, a reverse fault that places Paleozoic granite on Neogene sediments, varies in displacement from 0-2 km while the structural relief across the basin margin is 4 km. North of the fault, a 2 km thick panel of steeply-dipping to overturned sediments exhibits flexural shearing. This steep section is bounded by limbs of gently-dipping beds to the north and south. Northward, Neogene section is thrust over late Quaternary deposits in two younger episodes of faulting: the Akchop Hills Fault and the Aigyrdzal Hills Fault. Through 1:25,000 scale mapping I have demonstrated that of structural relief in the area is shared by fault propagation folding and faulting on a steep, reverse fault that shallows into a detachment. A complete geologic map of Kochkor, Kyrgyzstan is included with this thesis as a supplemental file.en_US
dc.identifier.urihttps://hdl.handle.net/1794/13426
dc.language.isoen_USen_US
dc.publisherUniversity of Oregonen_US
dc.rightsAll Rights Reserved.en_US
dc.subjectKochkoren_US
dc.subjectKyrgyzstanen_US
dc.subjectStructureen_US
dc.subjectTien Shanen_US
dc.titleGeneration of Structural Relief by Fault Propagation Folding, Tien Shan, Kyrgzstanen_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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