1887

Abstract

The agreement in the position of the Ordovician paleomagnetic poles from North America and from the Precordillera (Alcaparrosa F.) found when the former continent is rotated to a position close to western South America seems to support the hypothesis of an allochthonous origin for the Precordillera.

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/content/papers/10.3997/2214-4609-pdb.317.sbgf148
1989-11-20
2021-10-22
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.317.sbgf148
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