Brittle-viscous deformation cycles in the dry lower continental crust
Many rheological models of the lithosphere (based on “strength envelopes”) predict a weak aseismic lower crust below the strong brittle upper crust. An alternative view, based on the distribution of crustal seismicity, is that the lower crust could also be strong and seismic. It has been suggested t...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Copernicus Publications
2015
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Online Access: | http://hdl.handle.net/11577/3235361 http://meetingorganizer.copernicus.org/EGU2015/EGU2015-8946.pdf |