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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2008
DOI: 10.2110/pec.08.90.0421
EISBN: 9781565763180
... Abstract Detailed mapping of two wave-dominated deltaic parasequences in the Sunnyside Member (Upper Cretaceous BlackhawkFormation) in the Book Cliffs outcrop belt, Utah, U.S.A., reveals an intra-parasequencearchitecture that includes a clearly defined set...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2006
AAPG Bulletin (2006) 90 (7): 1121–1140.
...Roy Davies; John Howell; Ron Boyd; Stephen Flint; Claus Diessel Abstract The Sunnyside Member of the Upper Cretaceous Blackhawk Formation in the Book Cliffs of eastern Utah provides an ideal opportunity to investigate high-resolution sequence-stratigraphic correlation between shallow-marine...
FIGURES | View All (12)
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...
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: 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...
Journal Article
Journal: Economic Geology
Published: 01 November 1977
Economic Geology (1977) 72 (7): 1285–1320.
...T. Casadevall; H. Ohmoto Abstract The Sunnyside mine, in the Eureka mining district, San Juan County, Colorado, produces 700 tons/day of gold-silver-copper-lead-zinc-cadmium ore and is currently the State's leading gold producer (28,500 ounces in 1974). Production is from veins filling faults...
Journal Article
Published: 01 December 1933
American Mineralogist (1933) 18 (12): 513–527.
... and defining conditions of vein formation and that a preliminary study of the manganese minerals of the Sunnyside mine at Eureka may give further information on this problem, since the veins are noted for the large bodies of rhodonite associated with base-metal ores. Copyright © 1933 by the Mineralogical...
Journal Article
Journal: PALAIOS
Published: 01 January 2007
PALAIOS (2007) 22 (1): 1–2.
FIGURES
Journal Article
Published: 01 November 2004
Journal of Paleontology (2004) 78 (6): 1146–1153.
FIGURES
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
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...
Series: Reviews in Economic Geology
Published: 01 January 2020
DOI: 10.5382/rev.21.08
EISBN: 9781629495798
FIGURES | View All (16)
Journal Article
Published: 01 March 2011
Journal of the Geological Society (2011) 168 (2): 547–557.
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
FIGURES | View All (5)
Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5401-1.217
EISBN: 9780813754079
Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5401-1.217
EISBN: 9780813754079
Image
High-resolution stratigraphy of the upper <b>Sunnyside</b> Member–lower Castlegate...
Published: 15 March 2020
Figure 8. High-resolution stratigraphy of the upper Sunnyside Member–lower Castlegate Sandstone (C.Ss.) interval, Desert Siding (DS), Little Elliott (LE) Mesa, The Cove (TCv), and Middle Mountain (MM) regions. The inset map shows the approximate location of this west-to-east schematic section
Image
Examples of discontinuous intrashoreface shales from the <b>Sunnyside</b> Member o...
Published: 01 July 2014
Figure 5 Examples of discontinuous intrashoreface shales from the Sunnyside Member of the Blackhawk Formation. (A) 15 cm (5.9 in.) thick discontinuous bed (white triangles) of interlaminated carbonaceous shale and sand lenses near the base of the lower shoreface deposits of the Sunnyside S3
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