Published May 1990
| public
Book Section - Chapter
Geochemical modeling of a steeply dipping boundary between continental and oceanic-arc lithosphere, west-central Idaho
Abstract
The western margin of the Cretaceous Idaho Batholith intruded the boundary between accreted oceanic and terranes and the continental margin. The geochemistry of the plutonic rocks indicates that it is an abrupt, steeply dipping boundary which extends through the lithosphere.
Additional Information
© 1990 Geochemical Society.Additional details
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