Geochemical constraints on the provenance of pre-Mississippian sedimentary rocks in the North Slope subterrane of Yukon and Alaska

Author:

Nelson Lyle L.1,Strauss Justin V.2,Crockford Peter W.34,Cox Grant M.5,Johnson Benjamin G.6,Ward William7,Colpron Maurice8,McClelland William C.7,Macdonald Francis A.9

Affiliation:

1. Department of Earth and Planetary Sciences, Johns Hopkins University, 3400 N. Charles Street, Baltimore, Maryland 21218, USA

2. Department of Earth Sciences, Dartmouth College, HB6105 Fairchild Hall, Hanover, New Hampshire 03755, USA

3. Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel

4. Department of Geosciences, Princeton University, Princeton, New Jersey 08544, USA

5. Centre for Tectonics, Resources and Exploration (TraX), Department of Earth Sciences, The University of Adelaide, Adelaide, South Australia 5005, Australia

6. Department of Geology and Geography, West Virginia University, 98 Beechurst Avenue, Morgantown, West Virginia 26506, USA

7. Department of Earth and Environmental Sciences, University of Iowa, 115 Trowbridge Hall, Iowa City, Iowa 52242, USA

8. Yukon Geological Survey, P.O. Box 2703 (K-14), Whitehorse, Yukon, Y1A 2C6, Canada

9. Department of Earth Science, University of California, Santa Barbara, 1006 Webb Hall, Santa Barbara, California 93106, USA

Publisher

Geological Society of America

Reference130 articles.

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3. Ulungarat Formation—Type section of a new formation, headwaters of the Kongakut River, eastern Brooks Range;Anderson;Alaska Division of Geological and Geophysical Surveys Public Data File 91-4,1991

4. Anderson, A.V., Wallace, W.K., and Mull, C.G., 1994, Depositional record of a major tectonic transition in northern Alaska: Middle Devonian to Mississippian rift–basin margin deposits, upper Kongakut River region, eastern Brooks Range, Alaska, inThurston, D.K., and Fujita, K., eds., 1992 Proceedings, International Conference on Arctic Margins: Anchorage, Alaska, U.S. Department of the Interior, Minerals Management Service, p. 71–76.

5. Detrital zircon geochronology and provenance of the Neoproterozoic to Late Devonian Franklinian basin, Canadian Arctic Islands;Anfinson;Geological Society of America Bulletin,2012

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