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Goblin Valley

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Relay structure at Buckskin Spring near <span class="search-highlight">Goblin</span> <span class="search-highlight">Valley</span>. Oblique deformation ...
Published: 01 December 2005
Figure 14 Relay structure at Buckskin Spring near Goblin Valley. Oblique deformation bands in the wide overlap damage zone are present.
Image
Comparison of permeability values obtained from different approaches (plug,...
Published: 01 July 2009
Figure 7 Comparison of permeability values obtained from different approaches (plug, minipermeameter [mini-perm] and image-based measurements). Data are from cataclastic deformation bands (DB) in Goblin Valley. Note that data for clusters of deformation bands show lower permeability values; n
Image
Figure 1. (A) Compressive and (B) extensional deformation band stepover geo...
Published: 01 March 2006
Figure 1. (A) Compressive and (B) extensional deformation band stepover geometries as viewed in the mode II direction. Deformation bands are the light-toned positive relief structures. The sense of offset is determined from displaced cross-bedding. Photographs taken in the Goblin Valley region
Image
Synthetic diagrams summarizing the evolution of the deformation and its ass...
Published: 15 November 2019
Figure 13. Synthetic diagrams summarizing the evolution of the deformation and its associated processes and the generated fault rocks in the sandstone-dominated formations at Goblin Valley: (A) at the incipient stage of deformation (displacement [ D ] of ∼10 cm [∼3.9 in.]), (B) when both smearing
Image
(A) Location of the study site at the scale of Utah: San Rafael desert. (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
Image
Graph summarizing the permeability of the host rocks (HR) and their resulti...
Published: 15 November 2019
Figure 5. Graph summarizing the permeability of the host rocks (HR) and their resulting fault rocks as a function of the deformation mechanisms. The square data are the measurements at the Clashach Cove site; the circle data illustrate the measurements at the Goblin Valley site. The gray scale
Image
(A, B) Grain size distribution of the host rock sandstones at Clashach Cove...
Published: 15 November 2019
of the diameter in two dimensions because of the truncation effect (sampling effect is neglected), as suggested by Pelto (1952) . (C, D) Grain size distribution of the host rock sandstones at Goblin Valley. The grain size distribution is obtained through laser diffraction analysis. c Sst. = coarse sandstone; f
Image
Examples of geometry and spatial distribution of band sets formed as revers...
Published: 01 June 2016
Crans quarry (Provence, France). C: Normal shear band cluster adjacent to normal fault surface near Goblin Valley State Park (Utah, USA). D: Normal shear band cluster at the vicinity of two fault surfaces in the Boncavaï quarry (Provence, France). E: Histograms of number of band per meter versus
Image
Micro- and macrostructural observations and quantification of the deformati...
Published: 15 November 2019
Figure 11. Micro- and macrostructural observations and quantification of the deformation at the second exposure – Goblin Valley. (A) Graph displaying the quantification of the deformation along the length of the cluster of the 2.1-m (6.9-ft) fault offset including a layer of clay ( Figure 4E
Journal Article
Journal: AAPG Bulletin
Published: 15 November 2019
AAPG Bulletin (2019) 103 (11): 2731–2756.
...Figure 13. Synthetic diagrams summarizing the evolution of the deformation and its associated processes and the generated fault rocks in the sandstone-dominated formations at Goblin Valley: (A) at the incipient stage of deformation (displacement [ D ] of ∼10 cm [∼3.9 in.]), (B) when both smearing...
FIGURES | View All (14)
Image
Scanning electron microscopy of backscattered electrons imaging of the host...
Published: 15 November 2019
Figure 9. Scanning electron microscopy of backscattered electrons imaging of the host rocks at Goblin Valley, at the exposure 1 (A–C), and at the exposure 2 (D–F). (A) Orange fine-grained sandstone host rock (unit c 5 in Figure 4D ); 25% of the rock is made of oxide-bearing oolites crushed
Image
Micro- and macrostructural observations and quantification of the deformati...
Published: 15 November 2019
Figure 10. Micro- and macrostructural observations and quantification of the deformation at the first exposure – Goblin Valley. (A) Graph displaying the quantification of the deformation along the length of the cluster of the 6-m (19.7-ft) fault exposure including alternating thin layers
Image
A)  General Jurassic chronostratigraphic section on the Colorado Plateau, c...
Published: 01 July 2005
. Buck Tank; c) Lake Powell: 8. Lake Powell, 9. Antelope Island; d) San Rafael Swell: 10. Big Hole Fault; e) Capitol Reef: 11. Torrey, 12. Capitol Reef, 13. Goblin Valley, 14. Lower Bown's Reservoir, 15. Capitol Gorge, 16. Henry Mountains; f) Escalante: 17. Calf Creek, 18. Escalante River, 19. Spencer
Journal Article
Journal: GSA Bulletin
Published: 01 March 2006
GSA Bulletin (2006) 118 (3-4): 343–348.
...Figure 1. (A) Compressive and (B) extensional deformation band stepover geometries as viewed in the mode II direction. Deformation bands are the light-toned positive relief structures. The sense of offset is determined from displaced cross-bedding. Photographs taken in the Goblin Valley region...
FIGURES | View All (7)
Journal Article
Journal: Geosphere
Published: 01 December 2013
Geosphere (2013) 9 (6): 1562–1636.
... of several key incompatible trace elements like Rb, Nb, and Pb. Additional tuff of Goblin Knobs has been confirmed by 40 Ar/ 39 Ar and paleomagnetic data at sites GA and GB across Railroad Valley to the east in a north-trending horst just west of the main Quinn Canyon Range. About 4 km to the north...
FIGURES | View All (75)
Journal Article
Journal: Geology
Published: 01 June 2016
Geology (2016) 44 (6): 423–426.
... Crans quarry (Provence, France). C: Normal shear band cluster adjacent to normal fault surface near Goblin Valley State Park (Utah, USA). D: Normal shear band cluster at the vicinity of two fault surfaces in the Boncavaï quarry (Provence, France). E: Histograms of number of band per meter versus...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2006
AAPG Bulletin (2006) 90 (2): 177–192.
... on the anticlinal hinge of the East Kaibab monocline; Surprise Canyon on the Waterpocket fold; Pulpit arch east of Mount Hillers; and the San Rafael desert just north of Goblin Valley State Park ( Figure 2 ). These field sites were chosen because previous workers have identified and characterized cataclastic...
FIGURES | View All (10)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 2012
AAPG Bulletin (2012) 96 (5): 869–876.
... in the Goblin Valley area, located in southern Utah, between the two sites described by Solum et al. (2010) . In this area, large numbers of deformation bands are observed, not only in what can be defined as damage zones around small extensional faults, but also widely distributed between the faults ( Aydin...
FIGURES | View All (4)
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP459.4
EISBN: 9781786203403
... equal-area projection of poles to deformation bands in the Mollys Castle–Goblin Valley area, south Utah. Two maxima suggest an average dihedral angle of 47°. (b–d) from Entrada Sandstone in the Goblin Valley area, San Rafael Desert, Utah. In this work we present a review of deformation bands...
FIGURES | View All (19)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2009
AAPG Bulletin (2009) 93 (7): 919–938.
...Figure 7 Comparison of permeability values obtained from different approaches (plug, minipermeameter [mini-perm] and image-based measurements). Data are from cataclastic deformation bands (DB) in Goblin Valley. Note that data for clusters of deformation bands show lower permeability values; n...
FIGURES | View All (10)