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Articles
Grand Banks and J-Anomaly Ridge: A Geological Comparison
1 Atlantic Geoscience Centre, Bedford Institute of Oceanography, Dartmouth, Nova Scotia, Canada B2Y 4A2
Geological and geophysical evidence supports the hypothesis that the J-anomaly ridge was a part of the Grand Banks in (late) Early Cretaceous time. Revised on May 16, 1977
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Science. ISSN 0036-8075 (print), 1095-9203 (online)