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North Chickamauga Creek basin

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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1974
AAPG Bulletin (1974) 58 (9): 1838–1846.
... and configuration of the depositional basin of the clastic facies is appropriate. The prominent and relatively resistant arkosic units of the Notchy Creek facies and the Hawkins member yield reliable data concerning the provenance, process of sedimentation, and the environment of deposition. Field...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1972
AAPG Bulletin (1972) 56 (12): 2457–2458.
... certainty, as the top of the Copper Ridge. I call the top of the Knox Group at the top of the Joachim in Arkansas, and the top of the Wells Creek or Mascot in Tennessee. The introduction of the nearly obsolete term “Chickamauga” for the upper 3,000 ft of Ordovician rocks is as unfortunate...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1972
AAPG Bulletin (1972) 56 (12): 2459–2460.
... trends northward (as shown in Figure 14, Thomas, 1972 ). Possibly the precise location of the facies boundary may be somewhat farther west. The upper Chickamauga limestone unit thins southwestward from Tennessee to a minimum in north-central Mississippi (Mellen discussion; Thomas, 1972 , Figs. 4, 6...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1972
AAPG Bulletin (1972) 56 (1): 81–106.
... grades northward to limestone ( Fig. 4 ); and north of the Southward well (2–1), the top of the dolostone possibly descends stratigraphically northward. In the Central basin of Tennessee, parts of the Stones River Group (particularly Ridley and Murfreesboro Limestones) are dolomitic ( Wilson, 1949 , p...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1950
AAPG Bulletin (1950) 34 (4): 672–681.
... of the Sequatchie fold and the Potts Creek fault on the northwest mark the position of the shift. Areas of exceptionally disturbed rocks near the Emory River north and northeast of the north end of the Sequatchie anticline ( Fig. 2 ) were noted by Keith (1897 , p. 3) and by Glenn (1925 , pp. 334-35...
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Journal Article
Journal: Palynology
Published: 01 January 2008
Palynology (2008) 32 (1): 205–212.
... site is 8.5 km to the northeast of the JOY-2 site. Key to abbreviations: C R = Rome Formation; C C = Conasauga Group; O C K = Knox Group; O CH = Chickamauga Group. The Nolichucky Shale belongs to an alternating suite of shale-rich and carbonate-rich formations that comprise the Conasauga...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1938
AAPG Bulletin (1938) 22 (4): 416–430.
... arch. The oil occurs in a narrow belt and the gas in a somewhat broader belt, both of which gradually disappear toward the southwest. The oil fields increase in size and productiveness toward the northeast, the most productive field of all being at the extreme north end of the region on and near...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1946
AAPG Bulletin (1946) 30 (7): 1140–1191.
... of the Murfreesboro from well cuttings. His zone B consists of light gray to light tan calcilutite, showing “birdseye” ( Tetradium ) inclusions. According to Born 14 these beds are found interbedded with typical Murfreesboro in some places, and in others, as in Wells Creek Basin, are found interbedded...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1952
AAPG Bulletin (1952) 36 (1): 1–72.
... in North America and other continents. In North America a great U-shaped narrow shallow Athens basin is delineated from Newfoundland southwestward to Alabama, westward to Arkansas, Oklahoma, and Nevada, and northwestward through Idaho, British Columbia, and Yukon to Alaska, with Athens faunules shown...
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Journal Article
Published: 28 February 2017
Journal of Paleontology (2017) 91 (3): 493–511.
... (WL143); ( 3 ) SUI 139883 (WS16-1). Scale bar=2 mm. The Winneshiek Konservat-Lagerstätte was discovered in 2005 when geologists of the Iowa Geological Survey (IGS) were mapping the geology of the Upper Iowa River basin. During the field investigations, a local...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2014
GSA Bulletin (2014) 126 (5-6): 639–651.
... C. Tankard A. , eds., Sedimentary Basins and Basin-Forming Mechanisms: Canadian Geological Society of Petroleum Geologists Memoir 12 , p. 425 – 446 . Bethke C.M. Marshak S. , 1990 , Brine migrations across North America: The plate tectonics of groundwater : Annual Review...
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Series: GSA Field Guide
Published: 01 January 2015
DOI: 10.1130/2015.0039(03)
EISBN: 9780813756394
... Abstract Upper North Chickamauga Creek in Hamilton and Sequatchie Counties, Tennessee, is severely impacted by acid mine drainage (AMD) emanating from more than 15 abandoned coal mines in headwater tributaries. AMD is formed when pyrite and other sulfide minerals are exposed to air and water...
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Journal Article
Published: 05 June 2013
Geological Magazine (2014) 151 (2): 328–338.
... yield abundant brachiopods and bryozoans. At locality B02_45 (N 79.2295, E 97.96872) a sequence of grey massive detrital limestones interbedded with claystones ( Fig. 3 ) is exposed along the unnamed creek in the basin of the Kan'on River ( Fig. 1 ). Limestones yield...
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Journal Article
Published: 01 October 2017
Earth Sciences History (2017) 36 (2): 318–336.
... MD/WV     Chickamauga and Chattanooga National Military Park GA/TN Pea Ridge National Military Park AR Coronado National Memorial AZ Pecos National Historic Park NM Cumberland Gap National Historic Park KY/TN/VA Potomac Heritage National Scenic Trail Wash. D.C. MD/PA/VA Death...
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Journal Article
Published: 01 November 2005
Journal of Paleontology (2005) 79 (6): 1131–1142.
... of Cahabagnathus cooperi from southwest Nevada and Cahabagnathus craigi from north-central Arkansas as the newly discovered youngest species in this phylogeny. The two new species of Cahabagnathus recognized in this paper possess an anterior lobe on the anterolateral process in the stelliplanate element ( Fig...
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Journal Article
Journal: GSA Bulletin
Published: 01 August 2001
GSA Bulletin (2001) 113 (8): 1067–1078.
... are at present identified only in the region north and west of the Illinois Basin. The final episode of platform drowning lasted from the late Chatfieldian into the Richmondian and resulted in formation of the widespread and highly diachronous DS5 omission surface at the top of the Trenton. We suspect...
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Journal Article
Published: 01 November 2010
Journal of Sedimentary Research (2010) 80 (11): 943–954.
... that formed from clayey alluvium deposited on the floodplain of Chattanooga Creek ( Jackson 1982 ); the clay directly overlies Middle Ordovician limestone strata assigned to the Chickamauga Group ( Luther 1979 ). Up to 1–2 m of disturbed fill materials occur across the site. A total of 24 monitoring wells (12...
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Series: GSA Field Guide
Published: 29 March 2018
DOI: 10.1130/2018.0050(01)
EISBN: 9780813756509
... granted by R.C. Blakey. Figure 8. North America in the Late Ordovician; © Colorado Plateau Geosystems, 2017, permission for use granted by R.C. Blakey. Stratigraphy of the Sevier Foredeep The Sevier foredeep basin in eastern Tennessee comprises one of the thickest clastic sequences...
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Journal Article
Published: 01 November 2000
Journal of Paleontology (2000) 74 (6): 1122–1147.
... 30 sections in eastern North America and Baltoscandia, where the P. undatus – P. tenuis Zone boundary projects into B. alobatus Subzone based on K-bentonite bed correlation. Elements previously assigned to form-species of Oistodus are shown to be apparatus associates in coniform apparatuses...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1948
AAPG Bulletin (1948) 32 (5): 709–744.
... in the structural analysis of two major chains of the earth. The Appalachian system extends along the eastern side of the North American continent from Newfoundland to Alabama, a distance of 2,000 miles. It disappears on the northeast into the Atlantic Ocean and on the south is covered by Cretaceous...
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