CaltechAUTHORS
Published May 1990 | Version public
Book Section - Chapter Metadata-only

Geochemical modeling of a steeply dipping boundary between continental and oceanic-arc lithosphere, west-central Idaho

Creators

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

Identifiers

Eprint ID
48379
Resolver ID
CaltechAUTHORS:20140812-110611222

Dates

Created
2014-08-13
Created from EPrint's datestamp field
Updated
2019-10-03
Created from EPrint's last_modified field