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San Rafael Desert

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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 December 2009
Lithosphere (2009) 1 (6): 328–336.
... exposed low-volume basaltic intrusions, such as dikes, plugs, and domes, in a small area (200 × 100 m), which we refer to as the Carmel outcrop, in the San Rafael Desert, Utah. This locality ( Figs. 1A and 1B ) provides a unique opportunity to explore the mechanisms that govern the initiation of magma...
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(A) Location of the study site at the scale of Utah: <span class="search-highlight">San</span> <span class="search-highlight">Rafael</span> <span class="search-highlight">desert</span>. (B)...
Published: 15 November 2019
Figure 4. (A) Location of the study site at the scale of Utah: San Rafael desert. (B) Geological map (modified from Doelling et al., 2015 ) and local stratigraphic column (modified from Schultz and Fossen, 2008 ) of the two study exposures (red stars), northeast of the Goblin Valley State Park
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(a) Geologic map showing the studied locality (MC) in the <span class="search-highlight">San</span> <span class="search-highlight">Rafael</span> <span class="search-highlight">Desert</span>...
Published: 01 July 2009
Figure 3 (a) Geologic map showing the studied locality (MC) in the San Rafael Desert, Utah, and the location for sample UT-A. Modified from Doelling (2001) . (b) A picture from the locality where the MC samples were taken.
Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP299.3
EISBN: 9781862395473
...Abstract Abstract The geometry, orientation and distribution of deformation bands and fractures in eolian sandstones, siltstones and shales of the San Rafael Desert and Moab Fault area have been investigated. The results show that deformation bands, which are cataclastic in eolian sandstones...
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Deformation band in the Entrada Sandstone showing rapid changes in thicknes...
Published: 01 December 2007
Figure 7 Deformation band in the Entrada Sandstone showing rapid changes in thickness. San Rafael Desert, Utah.
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(a) Jointed deformation-band shear zone in the Jurassic Entrada Formation a...
Published: 01 February 2006
Figure 9 (a) Jointed deformation-band shear zone in the Jurassic Entrada Formation at the San Rafael Desert site. (b) Two sets of joints are evident in northeast-dipping deformation bands: a northeast-striking, vertical set (black poles) and a northwest-striking, gently southwest-dipping set
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Deformation-band cluster in the Entrada Sandstone showing rapid changes in ...
Published: 01 December 2007
Figure 9 Deformation-band cluster in the Entrada Sandstone showing rapid changes in thickness. San Rafael Desert, Utah.
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Characterization of the damage zone for a minor fault in layered sand–silts...
Published: 01 July 2007
Fig. 12.  Characterization of the damage zone for a minor fault in layered sand–siltstones of the Entrada Sandstone (San Rafael Desert). Band frequency varies from sandstone layer to sandstone layer, and is highest in the well-sorted, aeolian layers (1 and 4).
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Photomicrographs of two deformation bands, both showing rapid increase in p...
Published: 01 December 2007
Figure 8 Photomicrographs of two deformation bands, both showing rapid increase in porosity from the left to the right. Such variations decrease the effect of such structures to reduce permeability in a reservoir. (a) Entrada Sandstone, San Rafael Desert. (b) Nubian Sandstone, Tayiba Mines, Sinai.
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Map of southern Utah showing locations of field sites. 1 = Hillsdale Canyon...
Published: 01 February 2006
= Cottonwood South, also on the East Kaibab monocline; 4 = Surprise Canyon on the Waterpocket fold (WF); 5 = Pulpit arch east of Mount Hillers (MH) in the Henry Mountains; 6 = San Rafael Desert, adjacent to the San Rafael swell (SRS).
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Deformation band thickness v. displacement, plotted for different lithologi...
Published: 01 July 2007
Fig. 5.  Deformation band thickness v. displacement, plotted for different lithologies. Cataclastic deformation bands are from the Entrada Sandstone, San Rafael Desert, Utah. Data from disaggregation–phyllosilicate bands are from Jurassic sandstones in the Gullfaks Field reservoir, northern North
Series: GSA Special Papers
Published: 16 January 2018
DOI: 10.1130/2018.2533
EISBN: 9780813795331
... largely but not entirely correspond to formation or group names, were deposited during northward continental drift from tropical latitudes (fluvial, tidal, and nearshore marine Moenkopi and fluvial Chinle) through desert latitudes (the erg-dominated Glen Canyon and San Rafael) to temperate latitudes...
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Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5402-X.269
EISBN: 9780813754086
...Abstract Abstract Location . The San Rafael Swell is a major domal uplift in the northwestern Colorado Plateau and dominates the structure of east-central Utah. The San Rafael Reef site is on its eastern edge, approximately 13 mi (21 km) west of Green River, in Emery County, Utah (Fig. 1). 1...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1972
AAPG Bulletin (1972) 56 (3): 480–493.
... Tertiary sequence of the Santa Ynez Mountains accumulated. The wedge-shaped area, including the San Rafael Mountains, between the Sierra Madre trough and the Ventura basin, underwent uplift and erosion during Late Cretaceous and early Eocene time. During the late early Eocene, a marine transgression...
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Journal Article
Journal: Geology
Published: 01 August 2012
Geology (2012) 40 (8): 695–698.
..., this comparison is independent of the total number of volcanoes in each volcanic field, or their total areas. Distribution of conduits in the San Rafael region is compared with vent distribution in volcanic fields ( Table 1 ) including the nearby Black Rock Desert volcanic field, Utah, and the Springerville...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 2006
AAPG Bulletin (2006) 90 (2): 177–192.
...Figure 9 (a) Jointed deformation-band shear zone in the Jurassic Entrada Formation at the San Rafael Desert site. (b) Two sets of joints are evident in northeast-dipping deformation bands: a northeast-striking, vertical set (black poles) and a northwest-striking, gently southwest-dipping set...
FIGURES | View All (10)
Journal Article
Published: 01 March 2012
Journal of the Geological Society (2012) 169 (2): 123–126.
...–length scaling . Geology , 21 , 1107 – 1110 . Doelling H.H. 2001 . Geologic map of the Moab and eastern part of the San Rafael Desert 30′ × 60′ quadrangles, Grand and Emery Counties, Utah, and Mesa County, Colorado . Utah Geological Survey Map , 180 . Fossen H...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2009
AAPG Bulletin (2009) 93 (7): 919–938.
...Figure 3 (a) Geologic map showing the studied locality (MC) in the San Rafael Desert, Utah, and the location for sample UT-A. Modified from Doelling (2001) . (b) A picture from the locality where the MC samples were taken. ...
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Journal Article
Journal: Geology
Published: 01 November 2015
Geology (2015) 43 (11): 1023–1026.
.... Connor C.B. Kruse S.E. Connor L.J. Savov I.P. , 2009 , Evidence of small-volume igneous diapirism in the shallow crust of the Colorado Plateau, San Rafael Desert, Utah : Lithosphere , v. 1 , p. 328 – 336 , doi:10.1130/L61.1. Erlund E.J. Cashman K.V. Wallace P.J...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1927
AAPG Bulletin (1927) 11 (8): 785–808.
... in the region and made a reconnaissance of type localities of formations in the San Juan Mountain region and in San Juan River Valley. The writers in company examined typical sections of the rocks in San Rafael Swell and in Green River Desert. G. H. Girty identified the fossils collected from the Hermosa...
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