The nature of deformation in the middle crust - evidence from the Belmont domain, Grenville province, Southeatern Ontario /
Mid-crustal deformation of orogenic belts was investigated through studies of exhumed terrains in the Belmont Domain of the Composite Arc Belt deformed during the Grenvillian Orogeny. === The western study area shows a family of broad (~10 km) antiformal sheath structures with NNE-trending axial...
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| Format: | Others |
| Language: | en |
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McGill University
2002
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=78362 |