Limestones of western Newfoundland that magnetized before Devonian folding but after Middle Ordovician lithification
A positive fold test and a negative conglomerate test help determine when and how stable remanence was acquired in the Middle Ordovician Table Head Group limestones of the Port au Port Peninsula of Newfoundland. The limestones magnetized after lithification and incorporation as clasts into a Middle...
Published in: | Geophysical Research Letters |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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American Geophysical Union
1989
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Online Access: | https://research.library.mun.ca/6206/ https://research.library.mun.ca/6206/1/LIMESTONES.OF.WESTERN.NEWFOUNDLAND.pdf https://research.library.mun.ca/6206/3/LIMESTONES.OF.WESTERN.NEWFOUNDLAND.pdf https://doi.org/10.1029/GL016i001p00093 |