Generation of Structural Relief by Fault Propagation Folding, Tien Shan, Kyrgzstan
dc.contributor.advisor | Hopkins, Samantha | en_US |
dc.contributor.author | Paulson, Kathryn | en_US |
dc.date.accessioned | 2013-10-10T23:19:25Z | |
dc.date.available | 2013-10-10T23:19:25Z | |
dc.date.issued | 2013-10-10 | |
dc.description.abstract | The 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.uri | https://hdl.handle.net/1794/13426 | |
dc.language.iso | en_US | en_US |
dc.publisher | University of Oregon | en_US |
dc.rights | All Rights Reserved. | en_US |
dc.subject | Kochkor | en_US |
dc.subject | Kyrgyzstan | en_US |
dc.subject | Structure | en_US |
dc.subject | Tien Shan | en_US |
dc.title | Generation of Structural Relief by Fault Propagation Folding, Tien Shan, Kyrgzstan | en_US |
dc.type | Electronic Thesis or Dissertation | en_US |
thesis.degree.discipline | Department of Geological Sciences | en_US |
thesis.degree.grantor | University of Oregon | en_US |
thesis.degree.level | masters | en_US |
thesis.degree.name | M.S. | en_US |