STRATIGRAPHY AND STRUCTURE OF THE NORTHEASTERN DOONERAK WINDOW AREA, CENTRAL BROOKS RANGE, NORTHERN ALASKA
At the eastern terminus of the Doonerak Window four fault-bounded tectono-stratigraphic assemblages are recognized; they are from bottom to top: (1) lower Paleozoic phyllites, slates, and volcanic rocks (Apoon assemblage); (2) Mississippian imbricates consisting of conglomerates, shales, and limesto...
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| Format: | Others |
| Language: | English |
| Published: |
2007
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| Online Access: | http://hdl.handle.net/1911/16102 |