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Updated: Jul 13, 2026

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Un origen de inestabilidad litosférica para los basaltos de inundación del río Columbia y la elevación de las

T C Hales1, D L Abt, E D Humphreys

  • 1Department of Geological Sciences, 1272 University of Oregon, Eugene, Oregon 97403, USA. thales@uoregon.edu

Nature
|December 13, 2005
PubMed
Resumen

Los basaltos del río Columbia (CRB) se originaron cerca de las montañas Wallowa, no en la pista del punto caliente de Yellowstone. El descenso del manto y una raíz plutónica separada explican el magmatismo y la elevación de CRB.

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