Along-fault migration of the Mount McKinley restraining bend of the Denali fault defined by late Quaternary fault patterns and seismicity, Denali National Park & Preserve, Alaska

The tallest mountain in North America, Denali (formerly Mount McKinley, 6,190 m), is situated inside an abrupt bend in the right-lateral strike-slip Denali fault. This anomalous topography is clearly associated with the complex geometry of the Denali fault, but how this restraining bend has evolved...

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Veröffentlicht in:	Tectonophysics 2016-12, Vol.693, p.489-506
Hauptverfasser:	Burkett, Corey A., Bemis, Sean P., Benowitz, Jeff A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Banks (topography) Constraining Deformation Deformation mechanisms Denali National Park & Preserve Evolution Fault lines Faults Geologic mapping Geological faults Geological mapping Glacial outwash Holocene Mapping Migration National parks Outwash Pleistocene Quaternary Quaternary geology Quaternary geomorphology Restraining bend Seismicity Slip Slope Studies Thrust fault Thrust faults Topography Topography (geology) Transpressional tectonics
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