Evidence for deep crustal seismic rupture in a granulite-facies, intraplate, strike-slip shear zone, northern Saskatchewan, Canada

Author:

Orlandini Omero F.1,Mahan Kevin H.1,Williams Michael J.2,Regan Sean P.2,Mueller Karl J.1

Affiliation:

1. Department of Geological Sciences, University of Colorado, UCB 399, Boulder, Colorado 80309-0399, USA

2. Department of Geosciences, University of Massachusetts, 627 North Pleasant Street, 233 Morrill Science Center, Amherst, Massachusetts 01003-9297, USA

Publisher

Geological Society of America

Subject

Geology

Reference106 articles.

1. Seismogenic structure of a crystalline thrust fault: Fabric anisotropy and coeval pseudotachylyte–mylonitic pseudotachylyte in the Grizzly Creek shear zone, Colorado;Allen,2011

2. A seismogenic zone in the deep crust indicated by pseudotachylytes and ultramylonites in granulite-facies rocks of Calabria (southern Italy);Altenberger;Contributions to Mineralogy and Petrology,2013

3. Fossil earthquakes recorded by pseudotachylytes in mantle peridotite from the Alpine subduction complex of Corsica;Andersen;Earth and Planetary Science Letters,2006

4. A new garnet-orthopyroxene thermometer based on reversed Al2O3 solubility in FeO-Al2O3-SiO orthopyroxene;Aranovich;The American Mineralogist,1997

5. Garnets recording deep crustal earthquakes;Austrheim;Earth and Planetary Science Letters,1996

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