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Corrie Sandstone

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Journal Article
Published: 01 September 1991
Journal of Sedimentary Research (1991) 61 (5): 768–774.
... (6 to 72 m in thickness; mean = 22 m) is initiated by flat-bedded eolian sandstones (0.5 to 7.0 m in thickness; mean = 2.9 m) of amalgamated interdraa or interdune origin and is topped by cross-bedded draa or dune sandstones (3 to 70 m in thickness; mean = 18 m). The eolian sequence represents...
Journal Article
Journal: GSA Bulletin
Published: 01 November 1951
GSA Bulletin (1951) 62 (11): 1347–1370.
... from a different direction than either the Berea sandstone or the Corry sandstone. In northwestern Pennsylvania, the Bedford shale was found to be the same as White's Cussewago shale and Chadwick's Hayfield shale. In the vicinity of Meadville, Pennsylvania, the Bedford shale and the Berea sandstone...
Journal Article
Published: 01 November 2007
Scottish Journal of Geology (2007) 43 (2): 107–114.
...Colin K. Ballantyne; Adrian M. Hall; William Phillips; Steven Binnie; Peter W. Kubik Synopsis Geomorphological mapping provides evidence for two former low-level corrie glaciers on Hoy, both defined by end moraines. Five 10 Be exposure ages obtained from sandstone boulders on moraine crests fall...
FIGURES | View All (4)
Journal Article
Journal: GSA Bulletin
Published: 30 September 1925
GSA Bulletin (1925) 36 (3): 455–464.
... carefully described by Prosser, 5 whose work furnishes the foundation for the present writing. In northwestern Pennsylvania Dr. I. C. White described the following succession in Erie and Crawford counties, adjacent to Ohio and western New York : 6 Corry sandstone Cussewago shale Cussewago sandstone...
Journal Article
Published: 04 November 2019
Scottish Journal of Geology (2019) 55 (2): 135–140.
... of the Clyde Plateau Volcanic Formation (Strathclyde Group). Above this, the succession is dominated by siltstones and sandstones with subsidiary limestones. The most notable of the latter is the c . 10 m Corrie Limestone with its spectacular Gigantoproductus assemblages and other shallow-marine fossils...
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Journal Article
Published: 05 October 2011
Geological Magazine (2012) 149 (4): 578–589.
... displaying unconformable relationships between Tournaisian and Famennian (Upper Old Red Sandstone) or Dalradian rocks. These localities, which include Hutton's historical unconformity, are described in Jutras, Young & Caldwell ( 2011 ). They are all considered to have been located on the Corrie shoulder...
Journal Article
Journal: GSA Bulletin
Published: 01 March 2010
GSA Bulletin (2010) 122 (3-4): 323–335.
...Matthew J. Kohn; Sudip K. Paul; Stacey L. Corrie Abstract The lower Lesser Himalayan sequence marks the northern extremity of the exposed Indian plate, and is generally interpreted as a passive margin. Five lines of evidence, however, collectively suggest a continental arc setting: (1) igneous...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2011
GSA Bulletin (2011) 123 (9-10): 1863–1879.
...S.L. Corrie; M.J. Kohn Abstract Pressure-temperature-time (P-T-t) conditions of metamorphism have been determined in the Annapurna region of central Nepal that place new constraints on the structural and tectonic evolution of the Himalayan orogenic wedge. Peak P-T conditions increase structurally...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1949
AAPG Bulletin (1949) 33 (6): 841–847.
... to the deeper formations (Onondaga or deeper) as compared with 28 in 1947. Of these, two were drilled for gas storage purposes. Of the remainder, 9 were gas wells and 19 were dry holes. Two of the wells, located in Erie County, were completed as dry holes in the Corry Medina sand gas pool. They definitely...
FIGURES
Journal Article
Published: 01 August 2001
Quarterly Journal of Engineering Geology and Hydrogeology (2001) 34 (3): 269–281.
... of the existing land surface in the area. Elsewhere the ice front does not appear to have got beyond the north coast of Devon and Cornwall, although a till has been identified on the Isles of Scilly and a possible glacial corrie has been described on Exmoor. Beyond these limits, however, the SW region will have...
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Journal Article
Published: 19 July 2016
Scottish Journal of Geology (2016) 52 (1): 55–63.
.... At its maximum extent, the glacier formed a proglacial delta generating large volumes of meltwater that flowed over the rock sill of the present-day Falls of Lora. The confluence of glacial ice masses, flowing from the Pass of Brander and tributary corrie glaciers, created a complex glaciofluvial...
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Journal Article
Published: 07 March 2017
Journal of the Geological Society (2017) 174 (4): 646–654.
... calcrete cement in sandstone) follow similar stable isotopic trends. An aridification trend preceded the formation of each HRPCH occurrence, corroborating studies on modern equivalents that suggest that they develop in the more arid range of calcrete formation. The better constrained isotopic values...
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Journal Article
Published: 01 November 2003
Geological Magazine (2003) 140 (6): 627–647.
... Devonian non-marine sediments of the Old Red Sandstone (ORS) magnafacies. A minimum 3.5 km pre-tectonic thickness of ‘lost’ ORS is estimated in the southern Lake District and comparable thicknesses in North Wales and East Anglia. Tectonically driven subsidence of the underlying Avalonian crust is required...
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Series: GSA Special Papers
Published: 01 January 1990
DOI: 10.1130/SPE250-p1
... a remarkably complete stratigraphic section. The rock record begins with Upper Cambrian Dagger Flat Sandstone. Deposition of Upper Cambrian sand and shale in a shallow sea gave way during Ordovician to deposition of black shales interbedded with some sand and black chert, reflecting more restricted circulation...
Journal Article
Published: 10 July 2019
Scottish Journal of Geology (2019) 55 (2): 141–154.
... Sandstone Formation in Figure 4 , the Clyde Sandstone may lie directly on the Kinnesswood Formation. The Ballagan Formation is also missing at Corrie in NE Arran, where the Clyde Sandstone Formation is considered to lie directly on a thin development of Kinnesswood Formation ( Young & Caldwell 2012...
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Journal Article
Published: 01 September 1992
Journal of the Geological Society (1992) 149 (5): 689–692.
... be required locally; this is far in excess of the c. 6% maximum observed. Furthermore, aeolian sandstones from Corrie shore have simi- lar porosity and permeability to the Cock of Arran samples, they contain upto 2% volcanic lithic and opaque clasts but lack titanite cement (Van Panhuys-Sigler & Trewin 1990...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2012
GSA Bulletin (2012) 124 (7-8): 1278–1292.
... and chemistry, and detrital zircon U-Pb geochronology. Putative source rocks comprising locally exposed Grenville basement were analyzed for comparison. Samples studied are primarily arkosic to subarkosic siltstones, sandstones, and minor conglomerate. Ternary tectonic discrimination diagrams indicate...
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Series: GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0047(04)
EISBN: 9780813756479
...). Within the Tonoloway Limestone, the larger caves are developed in the lower member of the Tonoloway Limestone immediately below a bed of silica-cemented sandstone. In contrast, the larger caves in the Keyser Limestone are located preferentially in limestone beds containing stromatoporoid reefs, and some...
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Journal Article
Published: 01 January 1978
Journal of the Geological Society (1978) 135 (1): 51–56.
... and include those of both aeolian and fluvial origin. They include: 1. Lower Permian aeolian sandstones of the Arran (Corrie Sandstone), Mauchline, Thornhill, Loch- maben and Dumfries basins of SW Scotland; 2. Aeolian Lower Permian Penrith Sandstone, Eden Valley, NW England; 3. Fluvial St. Bees Sandstone...
Journal Article
Published: 25 March 2009
Geological Magazine (2009) 146 (3): 400–418.
... of Nameless Corrie in the east ( Figs 3 , 5 ). Evidence for formation of this sheet by extrusive pyroclastic processes is seen at three localities [NM 3775 9255; NM 3850 9270; NM 3888 9319]. The sheet is underlain by mesobreccia or pebbly sandstones ( Fig. 6 c), which pass either sharply or somewhat...