Cooling history of the St. Elias syntaxis, southeast Alaska, revealed by geochronology and thermochronology of cobble-sized glacial detritus

Author:

Falkowski Sarah1,Enkelmann Eva2,Drost Kerstin1,Pfänder Jörg A.3,Stübner Konstanze1,Ehlers Todd A.1

Affiliation:

1. Department of Geosciences; University of Tübingen; Tübingen Germany

2. Department of Geology; University of Cincinnati; Cincinnati Ohio USA

3. Department of Geology; TU Bergakademie Freiberg; Freiberg Germany

Funder

Deutsche Forschungsgemeinschaft

European Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference112 articles.

1. Detrital zircon ages from the Chugach Terrane, southern Alaska, reveal multiple episodes of accretion and erosion in a subduction complex;Amato;Geology,2010

2. Mesozoic and Early Cenozoic magmatic evolution of the Canadian Cordillera;Armstrong;Geol. Soc. Am. Spec. Pap.,1988

3. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation;Beaumont;Nature,2001

4. Extreme localized exhumation at syntaxes initiated by subduction geometry;Bendick;Geophys. Res. Lett.,2014

5. Berg , H. C. D. L. Jones D. H. Richter 1972 Gravina-Nutzotin Belt: Tectonic significance of an upper Mesozoic sedimentary and volcanic sequence in southern and southeastern Alaska U S Geol Surv Prof Pap 800D

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