Tectonic Growth of a Collisional Continental Margin: Crustal Evolution of Southern Alaska

Stratigraphy, depositional systems, and provenance of the Lower Cretaceous Kahiltna assemblage, western Alaska Range: Basin development in response to oblique collision
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Published:January 01, 2007
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CiteCitation
James L. Kalbas, Kenneth D. Ridgway, George E. Gehrels, 2007. "Stratigraphy, depositional systems, and provenance of the Lower Cretaceous Kahiltna assemblage, western Alaska Range: Basin development in response to oblique collision", Tectonic Growth of a Collisional Continental Margin: Crustal Evolution of Southern Alaska, Kenneth D. Ridgway, Jeffrey M. Trop, Jonathan M.G. Glen, J. Michael O'Neill
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The Kahiltna assemblage of southern Alaska crops out in an 800-km-long belt that forms the core of much of the rugged Alaska Range. New sedimentologic, provenance, and geologic mapping data suggest that the Kahiltna assemblage exposed in the western Alaska Range represents a late Early Cretaceous to Late Cretaceous marine basin that formed in response to oblique collision between a composite island-arc terrane and the Mesozoic continental margin of North America. The Kahiltna assemblage in the study area crops out in two belts located north and south of the Denali fault system. Measured stratigraphic sections show that the Kahiltna assemblage...
- absolute age
- Alaska
- Alaska Range
- Albian
- Aptian
- basins
- clastic rocks
- clasts
- conglomerate
- continental margin
- Cretaceous
- dates
- Denali Fault
- depositional environment
- detritus
- island arcs
- lithofacies
- lithostratigraphy
- Lower Cretaceous
- mapping
- Mesozoic
- nesosilicates
- North America
- orthosilicates
- provenance
- sandstone
- sedimentary rocks
- silicates
- suture zones
- tectonic elements
- terranes
- U/Pb
- United States
- uplifts
- Upper Cretaceous
- Wrangellia
- zircon
- zircon group
- Kahiltna Assemblage
- western Alaska Range