Indicadores paleocurrentes en los sedimentos de aguas profundas

Science (New York, N.Y.)
|March 30, 1979
PubMed
Resumen

Los investigadores estudiaron los sedimentos de aguas profundas en el Canal Vema para comprender las corrientes oceánicas pasadas. La textura de los sedimentos y la alineación de los granos magnéticos revelaron períodos de flujo de agua de fondo de alta velocidad y su dirección.

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