Formation of a metamorphic complex along an obliquely convergent margin: Structural and thermochronological evolution of the Chugach Metamorphic Complex, southern Alaska-Reference-Cited by-同舟云学术

Formation of a metamorphic complex along an obliquely convergent margin: Structural and thermochronological evolution of the Chugach Metamorphic Complex, southern Alaska

Published:2011-04 Issue:2 Volume:30 Page:n/a-n/a
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Gasser Deta,Bruand Emilie¹,Stüwe Kurt¹,Foster David A.²,Schuster Ralf³,Fügenschuh Bernhard⁴,Pavlis Terry⁵

Affiliation:

1. Department of Earth Science; University of Graz; Graz; Austria

2. Department of Geological Sciences; University of Florida; Gainesville; Florida; USA

3. Geological Survey of Austria; Vienna; Austria

4. Faculty of Geo- and Atmospheric Sciences; University of Innsbruck; Innsbruck; Austria

5. Department of Geological Sciences; University of Texas at El Paso; El Paso; Texas; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/tc/tc1102/2010TC002776/2010TC002776.pdf

Reference119 articles.

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3. Plate tectonic history of the northeast Pacific and western North America

4. The role of ridge subduction in determining the geochemistry and Nd-Sr-Pb isotopic evolution of the Kodiak batholith in southern Alaska;Ayuso;Tectonophysics,2009

5. The 50 Ma granodiorite of the eastern Gulf of Alaska: Melting in an accretionary prism in the forearc;Barker;J. Geophys. Res.,1992

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