Paleozoic supracrustal rocks near Cheticamp, Nova Scotia
Near Cheticamp, northwestern Cape Breton Island, a sequence of supracrustal rocks overlies and cuts granite previously dated at 530±44 million years, as veil as older, presumably Precambrian gneisses. Rhyolite dikes feeding the supracrustal sequence yielded zircons giving a U-Pb discordia age of 439...
| Published in: | Atlantic Geology |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Atlantic Geoscience Society
1982
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| Online Access: | https://journals.lib.unb.ca/index.php/ag/article/view/1392 |