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Transporte advectivo profundo de partículas litogénicas en la cuenca de Panamá

S Honjo, D W Spencer, J W Farrington

    Science (New York, N.Y.)
    |April 30, 1982
    PubMed
    Resumen

    En la cuenca de Panamá, el flujo de partículas litogénicas aumentó con la profundidad, principalmente debido a la arcilla beidellita. Esta arcilla smectita fue transportada horizontalmente desde la ladera continental a través de corrientes de agua media.

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