Home > NBMG Publications >

New!  Geologic map of the eastern flank of the northern Cortez Mountains, Eureka County, Nevada [MAP AND TEXT]
Geol E flank N Cortez Mountains


 
Alternative Views:


FREE DOWNLOADS

PDF
Geospatial PDF (learn more)

To buy paper copy, click "add to cart"
Price: $20.00

Product Code: OF2022-06

Format

Folded
Rolled--please submit rolled items as a separate order.

Qty:  
Description
 
Title: Geologic map of the eastern flank of the northern Cortez Mountains, Eureka County, Nevada

Author:
Russell V. Di Fiori and Sean P. Long
Year: 2022
Series: Open-File Report 2022-06
Version:
Format: sheet: 24 x 27.5 inches, color; text: 7 pages, color
Scale: 1:20,000

The Cortez Mountains are located in north-central Nevada, southwest of Carlin (fig. 1). Previous geologic mapping in this region (Smith and Ketner, 1978) and previous stratigraphic studies (e.g., Smith and Ketner, 1976; Suydam, 1988) have defined an extensive exposure of the Early Cretaceous Newark Canyon Formation (NCF) on the eastern flank of the northern Cortez Mountains. In this region of Nevada, there have been differing interpretations of the timing and style of contractional deformation associated with construction of the Cordilleran mountain belt, as well as the potential relationship of the NCF to this deformation. Smith and Ketner (1977) did not observe evidence for contractional deformation in the NCF, and interpreted that regional Mesozoic contractional deformation must have taken place prior to NCF deposition.

Alternatively, Vandervoort (1987) and Suydam (1988) interpreted that the NCF was deposited in isolated basins that formed in response to regional tectonism along the ‘Eureka thrust belt’ (also known as the Central Nevada thrust belt of Taylor et al. [1993, 2000]). The goal of this study is to present map data that illustrate field relations between the NCF and surrounding rock units. We present a new 1:20,000-scale geologic map of the eastern flank of the northern Cortez Mountains that covers ~42 km2 (a ~13 km north–south by ~4 km east–west distance), which covers the extent of exposure of the NCF (fig. 1). To illustrate the deformation geometry of the NCF relative to underlying and overlying rock units, we also present two retro-deformable cross sections. This report is meant to accompany Di Fiori et al. (2021), which characterizes the stratigraphic architecture, deposition timing, and deformation history of three NCF exposures in central Nevada, including the Cortez Mountains exposure. The following report provides descriptions of all rock and surficial units in the map area, with a focus on intraformational members of the NCF that we defined in our mapping, as well as the structural framework and geologic history of the map area and surrounding region.

Research was supported by the National Science Foundation and the U.S. Geological Survey National Cooperative Geologic Mapping Program under STATEMAP award number G20AC00390, 2020.

This map covers parts of these USGS 1:24,000-scale quadrangles: McCormack Spring and Palisade.

Suggested Citation:
Di Fiori, R.V., and Long, S.P., 2022, Geologic map of the eastern flank of the northern Cortez Mountains, Eureka County, Nevada: Nevada Bureau of Mines and Geology Open-File Report 2022-06, scale 1:20,000, 7 p.

© Copyright 2022 The University of Nevada, Reno. All Rights Reserved.