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Ruby River basin

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Journal Article
Published: 01 September 1981
Journal of Sedimentary Research (1981) 51 (3): 939–951.
...) marginal lacustrine-deltaic and fluvial-lacustrine environments; and 3) alluvial-meandering stream, braided delta-distributary system, and allivial fan environments. Within the basin, a central core of limestones and fine-grained clastics of the lacustrine facies is flanked on the north and west by coarse...
Journal Article
Published: 01 March 1976
Journal of Paleontology (1976) 50 (2): 345–346.
Journal Article
Published: 01 March 1975
Journal of Paleontology (1975) 49 (2): 422–423.
Series: GSA Memoirs
Published: 01 January 1961
DOI: 10.1130/MEM82-p1
... A flora from Tertiary fossiliferous shales of the upper part of the Ruby Basin in southwestern Montana is described. The intermontane lacustrine deposits consist of two phases with distinct floral assemblages. The composite flora comprises aquatic, riparian temperate deciduous- and coniferous...
Series: GSA Memoirs
Published: 01 January 1961
DOI: 10.1130/MEM82
Journal Article
Journal: Geosphere
Published: 25 September 2017
Geosphere (2017) 13 (6): 1901–1948.
... in tectonics and paleogeography took place between ca. 8–5 Ma and ca. 3 Ma, that included the extinction of the Knoll-Ruby and intrabasin basin fault systems followed by southward migration of significant tectonism away from the Snake River Plain, resulting in development of a set of modern normal faults...
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Book Chapter

Author(s)
Herman F. Becker
Series: GSA Memoirs
Published: 01 January 1961
Book Chapter

Author(s)
Herman F. Becker
Series: GSA Memoirs
Published: 01 January 1961
Book Chapter

Author(s)
Herman F. Becker
Series: GSA Memoirs
Published: 01 January 1961
Journal Article
Journal: PALAIOS
Published: 16 April 2020
PALAIOS (2020) 35 (4): 165–174.
... and its correlates were deposited in an even more extensive basin than the Grant (which would include the Fossil and Upper Ruby River basins), east of the Late Cretaceous–Paleogene Laramide rift system ( Stroup et al. 2008 ). Hanneman et al. (2003) and Hanneman and Wideman (2013) , while evaluating...
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Image
(A) Maps showing the locations of Rogerson graben, Knoll-Ruby fault system, Mesozoic plutons, and areas of documented downflexing of rocks along the margins of the Snake River Plain. The locations of faults in the Rogerson graben are after Andrews et al. (2008) and plutons are from Coats (1987). Distribution of faults in the area between the Contact pluton and the Rogerson graben is simplified from Coats (1987). Arrows representing areas and directions of downflexing are from McQuarrie and Rodgers (1998), Hough (2001), Rodgers et al. (2002), Michalek (2009), and Knott et al. (2016a, 2016b). Hinge of the flexural monocline adjacent to the Rogerson graben is from Knott et al. (2016b). Location of the western Snake River graben is from Wood and Clemens (2002). The shaded relief maps were produced from http://www.GeoMapApp.org/ and Ryan et al. (2009). Elevation is in meters above sea level. (B) Diagram comparing the timing of deposition versus erosion and faulting in the Ruby basin, the Knoll basin, and the Rogerson graben. See text for references and explanation. (B) Diagram comparing the timing of deposition versus erosion and faulting in the Ruby basin, the Knoll basin, and the Rogerson graben. See text for references and explanation.
Published: 25 September 2017
Figure 13. (A) Maps showing the locations of Rogerson graben, Knoll-Ruby fault system, Mesozoic plutons, and areas of documented downflexing of rocks along the margins of the Snake River Plain. The locations of faults in the Rogerson graben are after Andrews et al. (2008) and plutons are from
Image
(A) Maps showing the locations of Rogerson graben, Knoll-Ruby fault system, Mesozoic plutons, and areas of documented downflexing of rocks along the margins of the Snake River Plain. The locations of faults in the Rogerson graben are after Andrews et al. (2008) and plutons are from Coats (1987). Distribution of faults in the area between the Contact pluton and the Rogerson graben is simplified from Coats (1987). Arrows representing areas and directions of downflexing are from McQuarrie and Rodgers (1998), Hough (2001), Rodgers et al. (2002), Michalek (2009), and Knott et al. (2016a, 2016b). Hinge of the flexural monocline adjacent to the Rogerson graben is from Knott et al. (2016b). Location of the western Snake River graben is from Wood and Clemens (2002). The shaded relief maps were produced from http://www.GeoMapApp.org/ and Ryan et al. (2009). Elevation is in meters above sea level. (B) Diagram comparing the timing of deposition versus erosion and faulting in the Ruby basin, the Knoll basin, and the Rogerson graben. See text for references and explanation. (B) Diagram comparing the timing of deposition versus erosion and faulting in the Ruby basin, the Knoll basin, and the Rogerson graben. See text for references and explanation.
Published: 25 September 2017
Figure 13. (A) Maps showing the locations of Rogerson graben, Knoll-Ruby fault system, Mesozoic plutons, and areas of documented downflexing of rocks along the margins of the Snake River Plain. The locations of faults in the Rogerson graben are after Andrews et al. (2008) and plutons are from
Journal Article
Published: 01 January 2002
Rocky Mountain Geology (2002) 37 (1): 13–30.
... layers yield upwards of several hundred individuals per square foot. The fossil deposit has both lithologic and biotic similarities to paper shales containing insects and plants in the Upper Ruby River Basin, about 100 km to the south ( Becker, 1959 , 1960 , 1961 , 1966 , 1969 , 1972 ; Dorr...
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Journal Article
Journal: Geosphere
Published: 01 February 2012
Geosphere (2012) 8 (1): 1–27.
... foothills of the Sierra Nevada to the Ruby Mountains in northeastern Nevada, present-day distances of ∼280 km west and 300 km northeast of its source caldera. Corrected for later extension, the tuff flowed ∼200 km to the west, downvalley and across what is now the Basin and Range–Sierra Nevada structural...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 21 September 2020
Lithosphere (2020) 2020 (1): 2298288.
... River assemblage. These previously undated compressional structures are thought to be related to the final collapse of the Jura-Cretaceous basins and the tectonic burial of the Blanchard River assemblage resulting in amphibolite facies metamorphism. New in situ U-Th-Pb monazite ages record at least...
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Journal Article
Journal: Geosphere
Published: 01 February 2008
Geosphere (2008) 4 (1): 36–74.
.... The Elko basin is an extensive, elongate basin located between the Ruby Mountains and East Humboldt Range to the east and the Adobe Range and Piñon Range to the west. Its southern end is south of Jiggs along Huntington Creek, and it extends far to the north along the Marys River Valley (Fig. 10) . Small...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1970
AAPG Bulletin (1970) 54 (2): 285–312.
..., Hamilton-Elko, Ferguson, Pequop-Diamond Creek, Montello-Sublett, Ruby, and Park City basins are the more negative parts of the geosyncline, whereas several shelves and the Riepe Spring, Collville, Pakoon, and Kaibob platforms identify the less negative repositories. Starved basins of relatively short...
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Image
Correlation of high-resolution C-isotope stratigraphy from the Vocontian Basin of SE France (Herrle et al. 2004) with the C-isotope chemostratigraphy of the Cedar Mountain Formation at the Price River and Ruby Ranch Road sections. The curve from Herrle et al. (2004) is a ten-point moving average.
Published: 01 November 2010
Figure 15 Correlation of high-resolution C-isotope stratigraphy from the Vocontian Basin of SE France ( Herrle et al. 2004 ) with the C-isotope chemostratigraphy of the Cedar Mountain Formation at the Price River and Ruby Ranch Road sections. The curve from Herrle et al. (2004) is a ten-point
Image
Isopach map of Lower Cretaceous strata and generalized paleogeographic map of the Sevier thrust front and foreland-basin system in Utah and Colorado during the Albian, modified from Currie (2002). Note location of the Price River (PR) section in the area of the foredeep, and location of the Ruby Ranch Road (RRR) section in the area of the forebulge.
Published: 01 November 2010
Figure 3 Isopach map of Lower Cretaceous strata and generalized paleogeographic map of the Sevier thrust front and foreland-basin system in Utah and Colorado during the Albian, modified from Currie (2002) . Note location of the Price River (PR) section in the area of the foredeep, and location
Journal Article
Published: 01 May 2015
Canadian Journal of Earth Sciences (2015) 52 (7): 431–443.
... Lewes River – Stuhini arc in northwestern Stikinia (200–208 Ma, 216–220 Ma). When combined with other published age information, the ultramafic rocks in the Kluane Schist are interpreted as fragments of deeper arc-related mafic and ultramafic intrusive rocks introduced to the Kluane forearc basin...
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