Late Cenozoic Paleogeographic Evolution of Northeastern Nevada: Evidence from the Sedimentary Basins
Late Cenozoic paleogeographic evolution of northeastern Nevada: Evidence from the sedimentary basins Alan R. Wallace* U.S. Geological Survey, MS 176, Mackay School of Earth Sciences and Engineering, University of Nevada, Reno, Nevada 89557, USA Michael E. Perkins* Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112, USA Robert J. Fleck* U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA ABSTRACT lier faults are more pronounced east of the hot-spring deposits formed at and near the Tuscarora Mountains, possibly refl ecting a paleosurface in the Chimney, Ivanhoe, and Field and geochronologic studies of Neo- hanging-wall infl uence related to uplift of the Carlin basins as those basins were forming. gene sedimentary basins in northeastern Ruby Mountains-East Humboldt core com- The Neogene geologic and landscape evolu- Nevada document the paleogeographic and plex on the east side of the Elko basin. The tion had variable effects on all of these depos- geologic evolution of this region and the later faults are concentrated along the north- its, including uplift, weathering, supergene effects on major mineral deposits. The broad northwest–trending northern Nevada rift enrichment, erosion, and burial, depending area that includes the four middle Miocene west of the Tuscarora Mountains. The area on the events at any particular deposit. As basins studied—Chimney, Ivanhoe, Car- west of the rift contains major tilted horsts such, this study documents the importance of lin, and Elko, from west to east—was an and alluvium-fi lled grabens, and differential evaluating post-mineralization processes at upland that underwent prolonged middle extension between this more highly extended both regional and local scales when exploring Tertiary exposure and moderate erosion.
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