Shady Formation

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Journal Article
Published: 01 May 1982
Canadian Journal of Earth Sciences (1982) 19 (5): 1094–1098.
...David R. Kobluk Abstract Labyrinthus soraufi Kobluk 1979, previously known only from the upper Lower Cambrian Forteau Formation of southern Labrador, has been found within upper Lower Cambrian to lower Middle Cambrian Epiphyton mounds from the upper part of the Shady Dolomite in southwestern...
Series: GSA Special Papers
Published: 01 January 1982
DOI: 10.1130/SPE191-p35
... to the Precambrian and Lower Cambrian rocks of the Blue Ridge province on strike with the Talladega belt to the northeast. In the Borden Springs area, Cleburne County, Alabama, nappes of the Lower Cambrian Weisner and Shady Formations rest on younger Paleozoic rocks immediately northwest of the Talladega belt...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1985
AAPG Bulletin (1985) 69 (9): 1451–1452.
... of Shady Dolomite and 600 ft of Rome Formation above the St. Clair thrust fault. The Shady Dolomite, which contains several chert and shale beds up to 1 ft thick, is light gray to white, finely to coarsely crystalline, and thick bedded to massive. The upper part of the unit contains interbeds of grayish...
Journal Article
Published: 01 November 1992
Journal of Sedimentary Research (1992) 62 (6): 1023–1043.
...Roger J. Barnaby; J. Fred Read Abstract Outer platform carbonates of the Lower to Middle Cambrian Shady Dolomite, Virginia Appalachians, record a lengthy and complex diagenetic history, ranging from marine cementation to burial diagenesis during late Paleozoic overthrusting. Analysis...
Journal Article
Published: 01 March 1980
Journal of Sedimentary Research (1980) 50 (1): 91–116.
...R. W. Pfeil; J. F. Read Abstract Shelf edge, foreslope, and slope facies in the Lower to Middle Cambrian Shady Dolomite (600-1300 m thick) are exposed southeast of Austinville, southwestern Virginia, Valley and Ridge Province of the Appalachians. The Shady-Rome beds constitute an important type...
Journal Article
Published: 01 June 1976
Journal of Sedimentary Research (1976) 46 (2): 402–410.
...A. M. Thompson Abstract Probable algal fossil remains are identifiable in quartz-albite-biotite-chlorite-facies dolomitic marbles in the Lower Cambrian Shady Formation adjacent to the Alabama Piedmont. Organic origins were interpreted from distinctive recrystallization microfabrics...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1984
AAPG Bulletin (1984) 68 (4): 470.
... exposed along the leading edge of the metamorphic overthrust block. The Shady Formation becomes less dolomitic eastward, passing into dark, shaly limestone east of the carbonate bank edge. Rome-Conasauga siliciclastics change to carbonates eastward and northeastward. The Knox Group changes to limestone...
(A) Eastern outcrop&#x2F;road cut of the <b>Shady</b> Dolomite and Rome <b>Formation</b> in th...
Published: 11 May 2017
Figure 4. (A) Eastern outcrop/road cut of the Shady Dolomite and Rome Formation in the Shouns Prospect in the Mountain City window, Tennessee, showing zones of Mn oxidation within fracture and bedding planes, breccias, and nodules; (B) matrix-supported fracture/breccia fill (sample DR150124-A1
Journal Article
Journal: AAPG Bulletin
Published: 01 January 2006
AAPG Bulletin (2006) 90 (1): 1–20.
... during the deformational history of the rocks, providing a record of deformation under changing temperature and pressure conditions. These rocks probably initially entered the oil-generation window (80–140°C) during the Early Cretaceous formation of the Colville basin via thrust loading by the Brooks...
FIGURES | View All (13)
Journal Article
Journal: Economic Geology
Published: 01 December 1998
Economic Geology (1998) 93 (8): 1132–1152.
... McNamara Group is subdivided into four formations: the Shady Bore Quartzite, Riversleigh Siltstone, Termite Range Formation, and Lawn Hill Formation.The Shady Bore Quartzite comprises up to 460 m of sandstone and dolomitic siltstone, deposited in a marginal to shallow subaqueous environment...
Published: 01 January 1990
DOI: 10.5724/gcs.90.09.0099
EISBN: 978-1-944966-08-9
.... The Paleocene Midway formation overlies the mixed carbonate and clastic facies. It is composed of mainly shales with thin carbonate lenses and possibly dispersed organic matter. The sandy Wilcox formation of Late Paleocene-Early Eocene age overly the Midway. Other sand rich sediments were deposited during...
(A) In the <b>Shady</b> Dolomite in the Iron Mountain location of the Mountain Cit...
Published: 11 May 2017
Figure 5. (A) In the Shady Dolomite in the Iron Mountain location of the Mountain City window of Tennessee, interbedded Fe- and Mn oxide deposits are found in the fractured axes of existing folds. (B) Example of the interbedded Mn oxides and Fe oxyhydroxides showing porous and laminated
Journal Article
Journal: GSA Bulletin
Published: 01 January 1989
GSA Bulletin (1989) 101 (1): 42–54.
...-flow deposits at the base of the Hampton Formation. Deepening may have been enhanced by continued movement along listric faults throughout the incipient phase of passive-margin development. Most of the Hampton Formation and the overlying Erwin Formation and Shady Dolomite record pro-gradation...
Journal Article
Journal: Paleobiology
Published: 01 January 2004
Paleobiology (2004) 30 (1): 82–107.
... on the morphology and ecophysiology of these plants to infer early angiosperm function. With few exceptions, Amborella , Austrobaileyales, and Chloranthaceae share ecophysiological traits associated with shady, disturbed, and wet habitats. These features include low and easily light-saturated photosynthetic rates...
... on the southeast side of the window. The Stone Mountain fault was not recognized northeast of Troutdale, Virginia. The Shady Valley thrust sheet is continuous with the Blue Ridge thrust sheet. The ∼750 Ma Mount Rogers Formation occurs in three volcanic centers in the Blue Ridge thrust sheet. Basal clastic rocks...
FIGURES | View All (24)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1985
AAPG Bulletin (1985) 69 (9): 1440–1441.
... platform. The major lithostratigraphic units, all in the subsurface, are the Cambrian Mount Simon Sandstone, Shady Dolomite, Eau Clair Formation, Rome Formation, Conasauga Formation, and Kerbel Formation, and the Cambrian-Ordovician Knox Group. Stratigraphic interpretations generally show that the Sauk...
Series: Memoir, Memoir
Published: 01 January 2012
DOI: 10.1306/13331499M980271
EISBN: 9781629810201
... grading up into shelf siliciclastics) underlies the passive margin carbonates. Supersequence 2 consists of the Lower Cambrian Shady Dolomite–Rome-Waynesboro Formations. This is a shallowing-upward ramp succession of thinly bedded to nodular lime mudstones up into carbonate mud-mound facies, overlain...
FIGURES | View All (14)