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Uncoupling Coriolis Force and Rotating Buoyancy Effects on Full-Field Heat Transfer Properties of a Rotating Channel
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Overpressure and fluid flow in the new jersey continental slope: implications for slope failure and cold seeps

Dugan1, Flemings

  • 1503 Deike Building, Department of Geosciences, Penn State University, University Park, PA 16802, USA.

Science (New York, N.Y.)
|July 15, 2000
PubMed

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