The NE Pacific Ocean is considered the birthplace of many
fundamental ideas for modern plate tectonics theory. In this book
the orogenic belts of this region are discussed in a single,
internally consistent tectonic concept. Geological information is
considered the most reliable. Geophysical models are tested for
compatibility with observable geological data. The new concept
avoids force-fitting interpretations to preconceived assumptions
regarding accreted far-traveled terranes in the Cordillera and
continental-oceanic plate interactions in the entire region.
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