Provenance and Depositional Environment of Some Lower Mississippian Sediments, Cape George, Nova Scotia
The conglomerates of northern Cape George represent a tectonic block, thrusted from the north during the Carboniferous. Previous provenance studies of the Cape George alluvial fan sediments have not been done in great detail so that a probable source of the sediments had not be determined. During a...
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| Format: | Report |
| Language: | unknown |
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2022
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| Online Access: | http://hdl.handle.net/10222/82092 |