Tectonics, Fault Zones, and Topography in the Alaska–Canada Cordillera with a Focus on the Alaska Range and Denali Fault Zone

Author:

Caine Jonathan Saul,Benowitz Jeff A.

Publisher

Wiley

Reference48 articles.

1. Slip partitioning along a continuously curved fault: quaternary geologic controls on Denali fault system slip partitioning, growth of the Alaska range, and the tectonics of south‐Central Alaska;Bemis S.P.;Lithosphere,2015

2. Spatial variations in focused exhumation along a continental‐scale strike‐slip fault: the Denali fault of the eastern Alaska range;Benowitz J.A.;Geosphere,2011

3. Cenozoic tectono-thermal history of the Tordrillo Mountains, Alaska: Paleocene-Eocene ridge subduction, decreasing relief, and late Neogene faulting

4. Persistent long‐term (c. 24 Ma) exhumation in the eastern Alaska range constrained by stacked thermochronology;Benowitz J.A.;Geological Society, London, Special Publications,2014

5. Benowitz J. Roeske S. Regan S. et al. (2021)Large Scale Crustal‐Block Vertical Extrusion Between the Hines Creek and Denali Faults Coeval with Slip Localization on the Denali Fault since ca. 45 Ma: Hayes Range Alaska Geological Society of America Abstracts with Programs vol. 53.http://dx.doi.org/10.1130/abs/2021AM‐365121.

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