Grand Banks and J-Anomaly Ridge: A Geological Comparison

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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Bibliographic Details
Published in:Science (American Association for the Advancement of Science) 1977-09, Vol.197 (4308), p.1074-1076
Main Authors: Gradstein, F. M., Grant, A. C., Jansa, L. F.
Format: Article
Language:English
Subjects:
Basalt
Basement rocks
Carbonates
Geology
Limestones
Reflectors
Ridges
Rubber
Sediments
Subsidence
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Description
Summary:Geological and geophysical evidence supports the hypothesis that the J-anomaly ridge was a part of the Grand Banks in (late) Early Cretaceous time.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.197.4308.1074