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Topografía de discontinuidad del manto superior a partir de la heterogeneidad térmica y química

Nicholas Schmerr1, Edward J Garnero

  • 1Arizona State University, School of Earth and Space Exploration, Box 871404, Tempe, AZ 85287-1404, USA. nschmer@asu.edu

Science (New York, N.Y.)
|October 27, 2007
PubMed
Resumen

Investigando discontinuidades sísmicas debajo de América del Sur, este estudio revela límites de fase profundos vinculados a la heterogeneidad química de la zona de transición del manto y al potencial de fusión parcial. Estos hallazgos resaltan las contribuciones térmicas y químicas complejas a la estructura del manto superior.

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