Ophiolite emplacement along the Baie Verte-Brompton Line at Glover Island, western Newfoundland
The Glover Island Area of western Newfoundland spans the Humber-Dunnage Zone Boundary at the northern end of the Appalachian Orogen. Here a deformed ophiolitic pluton separates schists and gneisses (west) from mafic volcanic rocks (east). To the west, quartzo-feldspathic gneisses of the Cobble Cove...
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| Format: | Thesis |
| Language: | English |
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Memorial University of Newfoundland
1982
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| Online Access: | https://research.library.mun.ca/6744/ https://research.library.mun.ca/6744/1/DouglasAlanKnapp.pdf https://research.library.mun.ca/6744/3/DouglasAlanKnapp.pdf |