Fold fabrics and emplacement of an Archean granitoid pluton, Cleft Lake, Northwest Territories
The axial-plane foliation of early-phase folds in metagreywacke is commonly obliterated by a secondary, regional, crenulation cleavage or schistosity and quartz segregation layering. Nevertheless, remnants are preserved as quartz inclusion trails in biotite porphyroblasts. The trails deviate little...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1980
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Online Access: | http://dx.doi.org/10.1139/e80-032 http://www.nrcresearchpress.com/doi/pdf/10.1139/e80-032 |