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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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El movimiento cenozoico entre el este y el oeste de la Antártida

Cande1, Stock, Muller

  • 1Scripps Institution of Oceanography, La Jolla, California 92093-0215, USA. scande@ucsd.edu

Nature
|March 21, 2000
PubMed
Resumen

Una nueva investigación revela aproximadamente 180 km de separación entre el este y el oeste de la Antártida durante el Eoceno y el Oligoceno. Este desarrollo del sistema de grietas de la Antártida Occidental explica los eventos tectónicos clave y refina los modelos de movimiento de las placas globales.

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