Grand Banks and J-Anomaly Ridge: A Geological Comparison

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Science  09 Sep 1977:
Vol. 197, Issue 4308, pp. 1074-1076
DOI: 10.1126/science.197.4308.1074


Geological and geophysical evidence supports the hypothesis that the J-anomaly ridge was a part of the Grand Banks in (late) Early Cretaceous time.

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