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Singatse Range

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Journal Article
Journal: Lithosphere
Published: 01 June 2012
Lithosphere (2012) 4 (3): 187-208.
..., coincident with the development of an inboard component of plate-boundary transtensional deformation. Also, new age data from moderately tilted pre-extension volcanic rocks forming the lower part of the Tertiary stratigraphic section in the southern Singatse Range, west of the northern Wassuk Range, show...
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Series: GSA Special Papers
Published: 01 July 2008
DOI: 10.1130/2008.2438(09)
... Metamorphosed Triassic and Jurassic volcanic and sedimentary rocks have been mapped, described, and measured in the Singatse, Buckskin, and northern Wassuk Ranges near Yerington, west-central Nevada. Herein, we establish new formation names for these rocks and correlate them regionally...
Journal Article
Journal: Economic Geology
Published: 01 December 1992
Economic Geology (1992) 87 (8): 1963-2001.
...John H. Dilles; Marco T. Einaudi Abstract Surface exposures in the Singatse Range at the Ann-Mason deposit yield a nearly complete vertical cross section, from 1 to 6 km in paleodepth, through one of three porphyry Cu deposits genetically tied to the Middle Jurassic Yerington batholith. Detailed...
Journal Article
Journal: GSA Bulletin
Published: 01 January 2016
GSA Bulletin (2016) 128 (1-2): 223-238.
... paleointensity results determined using both the Coe modified Thellier method and the IZZI protocol on the medium-grained hornblende-biotite granite of the Middle Jurassic Shamrock batholith in the southern Singatse Range, western Nevada (USA). Previous zircon U-Pb dating gives an age of batholith emplacement...
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Journal Article
Journal: Geosphere
Published: 01 June 2011
Geosphere (2011) 7 (3): 756-773.
... of southern Oregon ( Fig. 1 ) ( Jordan et al., 2004 ; Lerch et al., 2008 ; Scarberry et al., 2010 ). In comparison, the western margin of the Basin and Range further south has undergone high-magnitude extension (>100%) such as in the Singatse-Wassuk region ( Proffett and Dilles, 1984 ; Surpless et al...
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Series: Society of Economic Geologists Guidebook Series
Published: 01 January 2000
DOI: 10.5382/GB.32
EISBN: 9781934969854
... in the Buckskin Range are exposed in cross-section due to 60 o –90 o W tilting produced by Miocene Basin and Range extension ( Proffett, 1977 ). The Buckskin Range exposures represent <1 km pale-odepth in contrast to the 1 to 7 km exposed in the Ann-Mason area of in the Singatse Range ( Dilles and Einaudi...
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Journal Article
Journal: GSA Bulletin
Published: 15 August 2018
GSA Bulletin (2019) 131 (1-2): 99-119.
...Sean P. Long Abstract The Basin and Range Province is a classic locality of continental extension, and it is ideal for analyzing factors that control the collapse of thickened orogenic crust. However, the magnitude and distribution of extension, which are critical parameters for this analysis...
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Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP458.8
EISBN: 9781786203397
...; Gans (1995) , Stockli et al. (2002) , Richardson & Seedorff (2015) Third 60 42 18 48 0.90 1.4 12.9 0.6 5.3 BA 11–8 3 5.56 × 10 −14 3 Tobin Range, Nevada First 66 41.5 25 48.5 0.88 0.5 49.0 0.7 36 R–(B?) 24.72–14.0 12.11 8.58 × 10 −14 JS, AB Gonsior...
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Journal Article
Journal: Geology
Published: 01 April 2009
Geology (2009) 37 (4): 371-374.
... sections. Northwestern Nevada— Colgan et al. (2006) ; Singatse-Wassuk Range— Surpless et al. (2002) and Proffett and Dilles (1984) ; central Nevada— Smith et al. (1991) ; Modoc-Owyhee Plateau— Wells and Heller (1988) . Actual values used for restoration are in parentheses. WLZ—Walker Lane zone. D...
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SAMPLE DATA AND  40 Ar/ 39 Ar AGES FOR ROCKS IN THE COAL VALLEY AREA AND SO...
Published: 01 June 2012
TABLE 1. SAMPLE DATA AND 40 Ar/ 39 Ar AGES FOR ROCKS IN THE COAL VALLEY AREA AND SOUTHERN SINGATSE RANGE, NEVADa
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40 Ar/ 39 Ar age-spectrum plots for rocks in the Coal Valley area and south...
Published: 01 June 2012
Figure 4. 40 Ar/ 39 Ar age-spectrum plots for rocks in the Coal Valley area and southern Singatse Range, Nevada. Uncertainties for all ages are at the 2σ level.
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40 Ar/ 39 Ar age-spectrum plots for rocks in the Coal Valley area and south...
Published: 01 June 2012
Figure 4. 40 Ar/ 39 Ar age-spectrum plots for rocks in the Coal Valley area and southern Singatse Range, Nevada. Uncertainties for all ages are at the 2σ level.
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Map showing location of Coal Valley relative to surrounding physiographic a...
Published: 01 June 2012
-shaded areas are (1) northern Wassuk Range studied by Anderson and Berger (2005) , (2) central Singatse Range where Proffett (1977) reported extreme extension, and (3) southern Singatse Range where Anderson and Berger (2005) reported minor extension.
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Figure 1. An approximate west to east cross section through the central Sin...
Published: 01 January 2002
Figure 1. An approximate west to east cross section through the central Singatse Range, just north of the Yerington Mine, Nevada. (A) As interpreted by Proffett and Dilles (1984 , section D−D′), steeper faults generally crosscut shallower faults (reproduced from Brady et al., 2000 , their Fig
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Figure 15. An approximately west to east cross section through the central ...
Published: 01 September 2000
Figure 15. An approximately west to east cross section through the central Singatse Range, just north of the Yerington Mine: (A) as interpreted by Proffett and Dilles (1984) , with steeper faults generally crosscutting shallower faults; (B) reinterpreted, assuming that steeper faults tend to merge
Journal Article
Journal: GSA Bulletin
Published: 01 July 2003
GSA Bulletin (2003) 115 (7): 788-816.
...Daniel F. Stockli; Trevor A. Dumitru; Michael O. McWilliams; Kenneth A. Farley Abstract The White Mountains represent the westernmost range of the central northern Basin and Range province. They are situated to the east of the unextended Sierra Nevada and represent a crustal block that is bounded...
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Journal Article
Journal: Geosphere
Published: 09 June 2017
Geosphere (2017) 13 (4): 1113-1132.
...-Pb thermal ionization mass spectrometry (TIMS) zircon ages (bulk separates) from plutonic and volcanic units from the Singatse and Buckskin Ranges, west of the Yerington mine, and showed that the ore-bearing porphyry dikes were emplaced between 169.4 and 168.5 Ma ( Dilles and Wright, 1988...
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(A) Reconstructed plan map of the Yerington batholith as exposed below the ...
Published: 01 November 2017
in the Singatse Range, showing projected geology from the Buckskin Range on the west and the Luhr Hill area on the east. The early McLeod Hill quartz monzodiorite (QMD) is a polyphase intrusion associated with small bodies of cumulate gabbro and was intruded by the Bear quartz monzonite and its upper granite
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Calderas and tuffs formed during the 34.4–34.0, 32.9–32.6, 31.5–28.8, and 2...
in > Geosphere
Published: 01 August 2013
—Gillis Range; GV—Gabbs Valley Range; P—Paradise Range; Pa—Pancake Range; R—Reveille Range; Ro—Royston Hills; S—Shoshone Mountains; Sh—Shoshone Range; Si—Singatse Range; St—Stillwater Range; T—Toquima Range; Te—Terrill Mountains; To—Toiyabe Range; V—Virginia Range;W—Wassuk Range.
Journal Article
Journal: Geosphere
Published: 01 August 2010
Geosphere (2010) 6 (4): 339-369.
... is the southeastern tributary of the Nine Hill paleovalley in the Singatse Range ( Fig. 1 ). Mapping at 1:12,000 supplemented by more than 30 km of drillhole data in the Yerington mining district document the paleovalley geometry, pinch outs of tuffs against topographic walls, 10 km width, and 1200 m depth (see...
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