1. Late Proterozoic–Paleozoic evolution of the Arctic Alaska–Chukotka terrane based on U-Pb igneous and detrital zircon ages: Implications for Neoproterozoic paleogeographic reconstructions;Amato;Geological Society of America Bulletin,2009
2. Age, chemistry, and correlations of Neoproterozoic–Devonian igneous rocks of the Arctic Alaska–Chukotka terrane: An overview with new U-Pb ages;Amato,2014
3. Ulungarat Formation–Type section of a new formation, headwaters of the Kongakut River, eastern Brooks Range, Alaska;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 of the 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;Anfinson;Canadian Arctic Islands: Geological Society of America Bulletin,2012