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Sunnyside Deposit

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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 645–646.
...Danny J. Wyatt Four major tar sand bodies in the Uinta basin were examined in terms of their depositional environments: (1) the Duchesne River and Mesaverde Formations at the Asphalt Ridge deposit near Vernal, Utah; (2) the Wasatch and Green River Formations at the Sunnyside deposit near Sunnyside...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 556.
...Jock A. Campbell The Sunnyside oil-impregnated sandstone deposit is a giant, exhumed oil field which occurs in the Green River Formation (Eocene), southwestern Uinta basin, Utah. The updip limit of the deposit has been eroded; thus, the precise mechanism of entrapment cannot be determined...
Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2008
DOI: 10.2110/pec.08.90.0421
EISBN: 9781565763180
... Sunnyside Member (Fig. 1 ; Young, 1955 ; Balsley, 1980 ; Howell and Flint, 2003 ), which crops out in the Book Cliffs of eastern Utah, was used as a basis for the work presented here. High-quality outcrops provide continuous exposure in both depositional dip and strike directions within the study area...
FIGURES | View All (14)
Series: AAPG Studies in Geology, AAPG Studies in Geology
Published: 01 January 1987
DOI: 10/1306/St25468C40
EISBN: 9781629811406
... Abstract Sandstones that crop out along the Roan Cliffs near Sunnyside, Utah, are estimated to contain approximately 6 billion barrels of bitumen, making it one of the largest deposits in the United States. Little is known of the geologic aspects, particularly sedimentology, mineralogy...
Journal Article
Journal: Economic Geology
Published: 01 August 2003
Economic Geology (2003) 98 (5): 1003–1018.
... and northern Patagonia mountains, Arizona. Two concealed porphyry copper deposits have been identified during past exploration, the Red Mountain and Sunnyside deposits, and related published hydrothermal alteration zoning studies allow the comparison of the results obtained from AVIRIS data to the more...
FIGURES | View All (10)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2006
AAPG Bulletin (2006) 90 (7): 1121–1140.
... ). The Sunnyside coal was deposited in a very large (>1800 km 2 ; >700 mi 2 ), continuous mire oriented approximately north-northeast–south-southwest, parallel to the shoreline of the Western Interior seaway ( Young, 1957 ; Doelling et al., 1979 ). Intensely rooted shoreface deposits underlie the seam...
FIGURES | View All (12)
Journal Article
Journal: Economic Geology
Published: 01 November 1977
Economic Geology (1977) 72 (7): 1285–1320.
... for Sunnyside sulfur. Isotopic studies of lead and rubidium-strontium suggest that metals in the Sunnyside ore fluids were scavenged from both Tertiary volcanic rocks and from the 1.4 to 1.8 b.y. Precambrian basement. Geological and geochemical studies suggest a model for Sunnyside ore deposition in which...
Series: Society of Economic Geologists Guidebook Series, Society of Economic Geologists Guidebook Series
Published: 01 January 1988
EISBN: 9781934969564
... Abstract The Sunnyside Hine is located in the Eureka r1ining District, San Juan County, Colorado. The tm1n of Silverton (pop. 600) lies approximately 8 miles. south of the mine (figure1) Bold outcrops of the Sunnyside, No Name, Washington and Belle Creole veins were discovered in the early...
Journal Article
Journal: Economic Geology
Published: 01 September 2014
Economic Geology (2014) 109 (6): 1667–1704.
... resource (60 Ma) that is associated with advanced, supergene-enriched argillic alteration. The youngest event includes the Sunnyside porphyry Cu-Mo system and a Cu-Mo breccia deposit at Red Hill (Four Metals mine), both of which formed in large-volume quartz monzonite, granodiorite, quartz monzonite...
FIGURES | View All (18)
Journal Article
Published: 01 November 2004
Journal of Paleontology (2004) 78 (6): 1146–1153.
.... Using data from the Permian and Triassic, we also examine the frequency of wood borings through time. All fossils occur within permineralized peat deposits in the Beardmore Glacier area, Queen Alexandra Range, central Transantarctic Mountains ( Taylor et al., 1989 ). The Late Permian peat is from...
FIGURES
Image
Simplified <b>depositional</b> dip cross section through the <b>Sunnyside</b> Member to s...
Published: 01 July 2006
Figure 6 Simplified depositional dip cross section through the Sunnyside Member to show the spacing of coal-sampling localities; see Figure 3B for position of localities in map view.
Image
—Intertonguing of late Cretaceous <b>deposits</b> between Castlegate and <b>Sunnyside</b>...
Published: 01 August 1957
Fig. 3. —Intertonguing of late Cretaceous deposits between Castlegate and Sunnyside Utah.
Series: Reviews in Economic Geology
Published: 01 January 2020
DOI: 10.5382/rev.21.08
EISBN: 9781629495798
... Abstract As the functionality and speed of 3-D geologic modeling software have improved over the last 30 years, it has become a core tool for identifying, understanding, and modeling the structural controls on ore deposits. This chapter attempts to summarize some of the key considerations...
FIGURES | View All (16)
Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5401-1.217
EISBN: 9780813754079
... the gneiss; it dips 35 degrees north. The fault cannot be traced into the upper part of the old alluvium and probably has been inactive since it was deposited, roughly 2,000 to 5,000 years ago (Crook and others,1978). Two of the earliest geologists to describe the San Gabriel Mountains (Davis, 1927; Miller...
Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5401-1.217
EISBN: 9780813754079
... the gneiss; it dips 35 degrees north. The fault cannot be traced into the upper part of the old alluvium and probably has been inactive since it was deposited, roughly 2,000 to 5,000 years ago (Crook and others,1978). Two of the earliest geologists to describe the San Gabriel Mountains (Davis, 1927; Miller...
Series: AAPG Special Publication, AAPG Special Publication
Published: 01 January 1991
DOI: 10.1306/SP548C8
EISBN: 9781629811161
... Abstract OBJECTIVE: During Day 2 of the field trip we will examine the stratigraphic architecture of the Kenilworth Member of the Blackhawk Formation and demonstrate how high-frequency cyclicity is expressed in wave-dominated shoreline deposits. Participants will be shown sedimentary facies...
Journal Article
Published: 01 March 2011
Journal of the Geological Society (2011) 168 (2): 547–557.
... of Ireland ( Fairon-Demaret 1986 , and references therein). The oldest woody axes distinct from Callixylon , the wood of archaeopteridalean progymnosperms, were described by Matten and his collaborators from Strunian deposits corresponding to the Retispora lepidophyta , probably LL, miospore zone...
FIGURES | View All (5)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP339.6
EISBN: 9781862395879
... The ‘Devonian plant hypothesis’ developed by Algeo and his collaborators in the past 15 years postulates a significant role of the vegetation in the series of biogeochemical events occurring in the Late Devonian (major biotic crises, extensive deposition of black shale horizons, atmospheric CO 2...
FIGURES | View All (5)
Image
(A) Correlation panel showing 29 outcrop logs through the <b>Sunnyside</b> Member ...
Published: 01 July 2006
Figure 3 (A) Correlation panel showing 29 outcrop logs through the Sunnyside Member and equivalent marginal- to nonmarine deposits; Mb = Member; PS = parasequence; OTZ = offshore transition zone; IVF = incised-valley fill. The total depositional dip extent of the section is approximately 50 km
Image
(A) Correlation panel showing 29 outcrop logs through the <b>Sunnyside</b> Member ...
Published: 01 July 2006
Figure 3 (A) Correlation panel showing 29 outcrop logs through the Sunnyside Member and equivalent marginal- to nonmarine deposits; Mb = Member; PS = parasequence; OTZ = offshore transition zone; IVF = incised-valley fill. The total depositional dip extent of the section is approximately 50 km