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Rye Patch area

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HyMap image mosaic of the Humboldt–<b>Rye</b> <b>Patch</b> <b>area</b> using bands at 2.2 μm, 0....
in > Geosphere
Published: 01 December 2011
Figure 2. HyMap image mosaic of the Humboldt–Rye Patch area using bands at 2.2 μm, 0.75 μm, and 0.55 μm as RGB. Greens indicate presence of vegetation; white is evaporates and surface alteration minerals; dark blue is water (Rye Patch reservoir); reds indicate soils enriched in iron-bearing
Journal Article
Journal: GSA Bulletin
Published: 01 August 1944
GSA Bulletin (1944) 55 (8): 921-950.
...CHARLES J. VITALIANO Abstract In the Rye Patch area in the west-central part of the Humboldt Range, Nevada, Triassic (?) limestones interbedded with silty layers have been intruded by igneous rocks, the principal type being a quartz monzonite. The quartz monzonite is surrounded on the north, east...
Journal Article
Journal: Geosphere
Published: 01 December 2011
Geosphere (2011) 7 (6): 1357-1368.
...Figure 2. HyMap image mosaic of the Humboldt–Rye Patch area using bands at 2.2 μm, 0.75 μm, and 0.55 μm as RGB. Greens indicate presence of vegetation; white is evaporates and surface alteration minerals; dark blue is water (Rye Patch reservoir); reds indicate soils enriched in iron-bearing...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1981
AAPG Bulletin (1981) 65 (8): 1414-1432.
... ( Fig. 4 ), is not particularly high along this southeastern lineament. The paucity of faults of any orientation along the northwestern segments of the system may be partly due to the general lack of detailed mapping in that area. Direction of movement along the Rye Patch lineament system...
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Journal Article
Published: 01 March 2000
Journal of the Geological Society (2000) 157 (2): 367-379.
...R. L. MASTERS; J. J. AGUE; D. M. RYE Abstract The carbon and oxygen systematics of rocks north of Stonehaven, Scotland were studied to provide new constraints on the nature and timing of metamorphic and post‐metamorphic fluid infiltration. Carbon and oxygen isotopic data were collected from...
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Journal Article
Journal: Economic Geology
Published: 01 January 2005
Economic Geology (2005) 100 (1): 131-148.
...C. L. Deyell; R. Leonardson; R. O. Rye; J. F. H. Thompson; T. Bissig; D. R. Cooke Abstract The Pascua-Lama high-sulfidation system, located in the El Indio-Pascua belt of Chile and Argentina, contains over 16 million ounces (Moz) Au and 585 Moz Ag. The deposit is hosted primarily in granite rocks...
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Journal Article
Journal: Economic Geology
Published: 01 May 2006
Economic Geology (2006) 101 (3): 503-522.
...Bat-Erdene Khashgerel; Robert O. Rye; Jeffrey W. Hedenquist; Imants Kavalieris Abstract The Oyu Tolgoi porphyry Cu-Au system in the South Gobi desert, Mongolia, comprises five deposits that extend over 6 km in a north-northeast–oriented zone. They occur in a middle to late Paleozoic arc terrane...
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Journal Article
Journal: Economic Geology
Published: 01 January 2003
Economic Geology (2003) 98 (1): 31-50.
...C. E. Everett; D. M. Rye; R. M. Ellam Abstract The Zn-Pb (-Ba) deposits of central Ireland are hosted by Lower Carboniferous Waulsortian limestone and Navan Group carbonate sediments. The deposits are located near the margins of subbasins in close association with extensional faults. The source...
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Journal Article
Journal: Economic Geology
Published: 01 September 2012
Economic Geology (2012) 107 (6): 1223-1249.
...Timothy S. Hayes; Gary P. Landis; Joseph F. Whelan; Robert O. Rye; Richard J. Moscati Abstract Ore formation at the Spar Lake red bed-associated strata-bound Cu deposit took place across a mixing and reaction zone between a hot oxidized metals-transporting brine and a reservoir of “sour” (H 2 S...
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Series: Geological Society, London, Engineering Geology Special Publications
Published: 01 January 2005
DOI: 10.5382/SP.11.03
EISBN: 9781629490359
..., the eruption of Vacas Heladas (or Tambo) Formation volcanic rocks at 12.7 to 11.0 Ma, prior to any known mineralization in the area. In the Pascua-Lama and Tambo deposits, stable isotope studies of alunite indicate that preore advanced argillic alteration is of magmatic-hydrothermal origin (cf. Rye et al...
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Journal Article
Journal: Economic Geology
Published: 01 December 2009
Economic Geology (2009) 104 (8): 1087-1110.
...Bat-Erdene Khashgerel; Robert O. Rye; Imants Kavalieris; Ken-ichiro Hayashi Abstract Late Devonian porphyry Cu-Au deposits within the Oyu Tolgoi mineral district, Mongolia, occur in a north-northeast–trending zone 22 km long. They are related to quartz monzodiorite intrusions, and hosted by augite...
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Journal Article
Published: 01 August 2010
Vadose Zone Journal (2010) 9 (3): 515-516.
... and connectivity of vegetation patches . Vadose Zone J . 9 : 561 – 572 (this issue). Robinson , D.A. , I. Lebron , and J.I. Querejeta . 2010 . Determining soil–tree–grass relationships in a California oak savanna using eco-geophysics . Vadose Zone J . 9 : x528 – 536 (this issue...
Journal Article
Published: 01 August 2010
Vadose Zone Journal (2010) 9 (3): 548-560.
... differences in patterns and quantity of use. The work supports the premise of two vadose zone water pools that have vastly different ecological and hydrological function. ET, evapotranspiration LAI, leaf area index Recently, Ryel et al. (2008) proposed a new conceptual model for plant water use...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2016
GSA Bulletin (2016) 128 (1-2): 284-314.
... component. The other branch (mid-valley fault) lies within the Indus Valley and is very linear, as highlighted on various satellite images ( Fig. 3 ) by vegetation patches fed by small springs. It is mainly strike-slip, with vertical motion due to local fault bends responsible for the formation of pressure...
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Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2001
DOI: 10.5382/SP.08.09
EISBN: 9781629490328
... zones along the Zuloaga vein. The illite-smectite zone consists of illite, smectite, and interstratified illite/smectite and occurs restricted to the upper portions of the vein above the orebodies. Patches of kaolin alteration also occur in this high-level environment. The productive mineralized zone...
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Journal Article
Published: 01 July 2004
European Journal of Mineralogy (2004) 16 (4): 631-640.
... immolation of ritual offerings took place. The formation of this unusually P-rich olivine is thought to be due to incongruent melting of biotite through a reaction such as biotite + quartz = olivine + Ti-magnetite + K-rich melt. During partial melting, foamy patches of dark glassy material formed...
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Journal Article
Journal: Economic Geology
Published: 01 December 2011
Economic Geology (2011) 106 (8): 1365-1398.
... of various types within an area of ~25 km 2 , including the Far Southeast porphyry Cu-Au deposit, the Lepanto high sulfidation epithermal Cu-Au deposit, the Victoria intermediate sulfidation epithermal Au-Ag vein deposit, the Teresa epithermal Au-Ag vein deposit, the Guinaoang porphyry Cu-Au deposit...
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Journal Article
Journal: Economic Geology
Published: 01 November 2014
Economic Geology (2014) 109 (7): 1929-1942.
...Bayaraa Batkhishig; Tsuchiya Noriyoshi; Greg Bignall Abstract The Shuteen area is located in the Gurvansaikhan island arc terrane of South Mongolia. It contains a large domain of intensely developed silicic and advanced argillic alteration that has strongly affected the adakitic volcanoplutonic...
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Journal Article
Journal: Economic Geology
Published: 01 June 2008
Economic Geology (2008) 103 (4): 783-799.
...N. I. Basuki; B. E. Taylor; E.T.C. Spooner Abstract The Bongara area, northern Peru, contains Mississippi Valley-type (MVT) Zn-Pb mineralization hosted in Late Triassic-Jurassic carbonate rocks of the Pucará Group. Mineralization is interpreted to have formed during the Late Cretaceous Peruvian...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1989
AAPG Bulletin (1989) 73 (2): 182-194.
... magnetization in the area. Elsewhere, anomalous magnetization in sedimentary rocks near hydrocarbon accumulations has been attributed to hydrocarbon-engendered magnetic minerals, but magnetization of the Preuss is controlled by detrital magnetite. Evidence of a detrital origin for magnetite includes (1...
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