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Discontinuidad isotópica lateral en la corteza inferior: un ejemplo de la Antártida

R I Kalamarides, J H Berg, R A Hank

    Science (New York, N.Y.)
    |September 4, 1987
    PubMed
    Resumen

    La investigación de los granulitos de la corteza inferior antártica revela una significativa discontinuidad de composición y edad. Este límite geológico, identificado a través de isótopos de estroncio y oxígeno, puede indicar una antigua sutura debajo de las montañas transantárticas.

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