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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Western Europe
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United Kingdom
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Great Britain
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Scotland
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Moray Firth (1)
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United States
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Arizona
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Navajo County Arizona
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Holbrook Arizona (1)
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Yavapai County Arizona (1)
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geologic age
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Mesozoic
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Triassic (1)
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Paleozoic
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Permian
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Coconino Sandstone (1)
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minerals
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silicates
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framework silicates
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silica minerals
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quartz (1)
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Primary terms
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Europe
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Western Europe
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United Kingdom
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Great Britain
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Scotland
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Moray Firth (1)
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Mesozoic
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Triassic (1)
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Paleozoic
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Permian
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Coconino Sandstone (1)
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petrology (1)
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sedimentary rocks
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clastic rocks
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sandstone (1)
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sedimentary structures
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planar bedding structures
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bedding (1)
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United States
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Arizona
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Navajo County Arizona
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Holbrook Arizona (1)
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Yavapai County Arizona (1)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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sandstone (1)
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sedimentary structures
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sedimentary structures
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planar bedding structures
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bedding (1)
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A Methodology For Disaggregation and Textural Analysis of Quartz-cemented Sandstones
Preliminary assessment of the petrology of the Hopeman Sandstone (Permo-Triassic), Moray Firth Basin, Scotland
Garden of the Gods at Colorado Springs: Paleozoic and Mesozoic sedimentation and tectonics
Abstract Exposed along the southeast flank of the Colorado Front Range are rocks that beautifully illustrate the interplay of sedimentation and tectonics. Two major range-bounding faults, the Ute Pass fault and the Rampart Range fault, converge on the Garden of the Gods region west of Colorado Springs. Cambrian through Cretaceous strata upturned by these faults reveal in their grain compositions, textures, and bed-forms radically different styles of sedimentation. The Cambrian/Ordovician marine transgressive deposits appear to have come to rest on a passive and tectonically inactive craton. In contrast, coarse-grained Pennsylvanian/Permian marine deposits of the Fountain Formation and Lyons Sandstone reveal deposition by suspension and tractive currents in a very dynamic tectonic setting. These styles are contrasted with the alternating eustatics of the Western Interior Seaway which led to the local Cretaceous section. Finally, the powerful imprint of the Laramide orogeny is evident in the sandstone dikes of Sawatch Sandstone which are found within the hanging wall of the Ute Pass fault.