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Showing 1 to 1 of 1 for “"Robert D. Conrad (Ship) Cruise RC2408"”.
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Cenozoic geology of the continental slope and rise off western Nova Scotia
The outer continental margin of Nova Scotia is divided by a diapir province, 40-110 km wide and ~1000km long, that trends subparallel to the shelf edge along the upper continental rise and slope. The growth pattern for a small region of this margin (61°-64°W) during the Late Cretaceous and Cenozoic …