Strain partitioning in an obliquely convergent orogen, plutonism, and synorogenic collapse: Coast Mountains Batholith, British Columbia, Canada

Author:

Andronicos Christopher L.,Chardon Dominique H.,Hollister Lincoln S.1,Gehrels George E.2,Woodsworth Glenn J.3

Affiliation:

1. Department of Geosciences; Princeton University; Princeton; New Jersey; USA

2. Department of Geosciences; University of Arizona; Tucson; Arizona; USA

3. Geological Survey of Canada; Vancouver; British Columbia; Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference64 articles.

1. Anderson , E. M. The Dynamics of Faulting and Dyke Formation With Applications to Britain Oliver and Boyd White Plains, N. Y. 1959

2. Kinematics and tectonic significance of transpressive structures within the Coast plutonic complex, British Columbia;Andronicos;J. Struct. Geol.y,1999

3. Phase relations among greenschist, epidote-amphibolite, and amphibolite in a basaltic system;Apted;Am. J. Sci.,1983

4. Mesozoic and early Cenozoic magmatic evolution of the Canadian Cordillera

5. Ductile and brittle shortening, extension-parallel folds and maintenance of crustal thickness in the central Aegean (Cyclades, Greece);Avigad;Tectonics,2001

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