Geology, Petrology, and Paleomagnetism of Eocene Basalts from the Black Hills, Washington Coast Range
Geologic mapping in the Black Hills area strongly suggests that the middle Eocene basalts of the Crescent Formation and over- lying upper Eocene and Oligocene sedimentary rocks constitute a structurally coherent terrane that is bounded by northeast- and northwest-trending faults. I interpret the Bla...
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Western Washington University
1980
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| Online Access: | https://dx.doi.org/10.25710/ks8q-yd48 https://cedar.wwu.edu/wwuet/660 |