The New World Island Complex and its relationships to nearby formations, north-central Newfoundland
The New World Island Complex consists of chaotically mixed volcanic and sedimentary rocks in a 1 km wide belt that extends 30 km southwestward from Cobbs Arm, on eastern New World Island, centrally located in the Dunnage Zone of the Newfoundland Appalachians. The complex comprises four lithic units,...
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| Format: | Thesis |
| Language: | English |
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Memorial University of Newfoundland
1983
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| Online Access: | https://research.library.mun.ca/6916/ https://research.library.mun.ca/6916/1/DouglasNormanReusch.pdf https://research.library.mun.ca/6916/3/DouglasNormanReusch.pdf |
| Summary: | The New World Island Complex consists of chaotically mixed volcanic and sedimentary rocks in a 1 km wide belt that extends 30 km southwestward from Cobbs Arm, on eastern New World Island, centrally located in the Dunnage Zone of the Newfoundland Appalachians. The complex comprises four lithic units, locally preserved in partial stratigraphic sections: Squid Cove Volcanics - basalts (non-orogenic tholeiites), autoclastic breccias, red shale, limestone, pyroclastic breccias and tuffs (Arenigian to Llandeilian); Cobbs Arm Limestone (Llandeilian); Rodgers Cove Shale - interbedded black shale and chert (Caradocian); and Muddy Cove Clastics - quartzitic greywackes, shales, polymictic conglomerates, and shaly conglomeratic breccias (Ashgillian to Llandoverian). -- Imbricated slices of competent volcanic rocks over 3 km long are separated by mylonitic and clastic shear zones. Intervening sedimentary slices contain boudinaged interbeds (1 cm to 100 m across) and tight fold hinges. These pass laterally into melange with discrete blocks of volcanic rocks, sandstones, and locally black shale in a sedimentary matrix. The blocks have sheared margins in places, and one large slab of Ordovician limestone is deeply penetrated by Silurian shale. Angular fragments in shaly conglomeratic breccias include black shale and limestone derived from the local stratigraphic section in adjacent fault blocks; one limestone clast is inhomogeneously deformed. -- The New World Island Complex is followed to the northwest by sandstones and conglomerates (Crow Head Formation) of Upper Ordovician to Silurian age. These are locally continuous with Caradocian black shale and older rocks in the complex. Farther northwest, pre-Caradocian volcanic rocks like those in the New World Island Complex (Clarkes Cove Volcanics) are unconformably overlain by coarse Silurian conglomerates (Indian Cove Formation) in another structural slice. The New World Island Complex structurally overlies Silurian conglomerates (Milliners Arm Formation) to the southeast. ... |
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