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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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Seafloor spreading along the Kula-Farallon plate boundaries may be the explanation for geographic separation and different ages of the submarine basalts in western Oregon-Washington. Eocene strata of the Columbia arc are interpreted to be Tertiary seafloor that was wedged between the Juan de Fuca and North American plates when, in early Refugian time, subduction changed from its Mesozoic-early Tertiary location to the present location.
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