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Oswego Limestone

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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1965
AAPG Bulletin (1965) 49 (9): 1561.
...W. E. Richardson Abstract The Oswego is the oldest and most widespread limestone unit of the Marmaton Group. The Marmaton is the oldest succession of Pennsylvanian carbonates that are indigenous to the shelf area of the western Mid-Continent. The Oswego Limestone occurs over most of northern...
Image
—Subsurface maps on <span class="search-highlight">Oswego</span> <span class="search-highlight">limestone</span> and Arbuckle <span class="search-highlight">limestone</span>. Contours on Os...
Published: 01 December 1930
FIG. 6. —Subsurface maps on Oswego limestone and Arbuckle limestone. Contours on Oswego are on base of member.
Image
—Representative shelf-to-basin cross section of the <span class="search-highlight">Oswego</span> <span class="search-highlight">limestone</span>, Marma...
Published: 01 April 1994
Figure 2 —Representative shelf-to-basin cross section of the Oswego limestone, Marmaton Group (undivided), Cleveland formation, and Kansas City Formation. Regional lithostratigraphic and sequence stratigraphic correlations presented in this report emphasize the dominantly siliciclastic section
Image
—Structure of base of <span class="search-highlight">Oswego</span> <span class="search-highlight">limestone</span>, Noble County, Oklahoma, showing loc...
Published: 01 August 1971
Fig. 14. —Structure of base of Oswego limestone, Noble County, Oklahoma, showing location of four stratigraphic profiles (modified after Scott, 1970 ).
Image
Type III. <span class="search-highlight">Limestone</span>—dense matrix and vuggy porosity. Pennsylvanian, <span class="search-highlight">Oswego</span> ...
Published: 01 March 1966
Fig. 6. Type III. Limestone—dense matrix and vuggy porosity. Pennsylvanian, Oswego Limestone, Dewey County, Oklahoma, × 2.5.
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Generalized cross section ( AAʹ ), showing beds from Arbuckle <span class="search-highlight">limestone</span> to ...
Published: 01 September 1941
Fig. 2. Generalized cross section ( AAʹ ), showing beds from Arbuckle limestone to Oswego limestone.
Image
—Areal distribution of component parasequences of the Marmaton lowstand sys...
Published: 01 April 1994
Figure 10 —Areal distribution of component parasequences of the Marmaton lowstand systems tract (P1–P5) and transgressive systems tract (P6). Boundaries of Oswego limestone buildup mark two physiographic breaks in the Oswego shelf platform; the eastern break coincides with the inferred early
Image
Isopach map of the interval from the top of the Mississippian <span class="search-highlight">limestone</span> to ...
Published: 01 January 2001
Figure 12 Isopach map of the interval from the top of the Mississippian limestone to the base of the Oswego limestone (the Cherokee interval) in the east-central part of the study area showing southward thickening that may control production.
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(A) Seismic cross section CC′ and (B) seismic cross section DD′. Both cross...
Published: 01 December 2021
Figure 15. (A) Seismic cross section CC′ and (B) seismic cross section DD′. Both cross sections are flattened on the Verdigris Limestone (yellow lines). Arrows mark the position of the Red Fork-Skinner horizon. Green line is Oswego limestone; blue is Prue interval shale; turquoise
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Well R synthetic seismogram using the seismic amplitude data. The correlati...
Published: 07 August 2013
Figure 15. Well R synthetic seismogram using the seismic amplitude data. The correlation was done using a 250-ms window centered at 1800 ms. The correlation coefficient is 70%. Orange marker corresponds to the Oswego Limestone. The yellow marker corresponds to the Inola Limestone, and the green
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Well S synthetic seismogram using the seismic amplitude data. The correlati...
Published: 07 August 2013
Figure 16. Well S synthetic seismogram using the seismic amplitude data. The correlation was done using a 300-ms window centered at 1800 ms. The correlation coefficient is 70%. The orange marker corresponds to the Oswego Limestone. The pink marker corresponds to the base of the Pink Lime
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—Diagrammatic section across Bartlesville area; based on wells listed  Tabl...
Published: 01 September 1975
, Hogshooter Formation; Po Oswego Limestone; Cm , Mississippian rocks; Oa , Arbuckle rocks; Pε , Precambrian rocks.
Image
—Regional west-east, dip-oriented cross section AA′ of the central part of ...
Published: 01 April 1994
Figure 7 —Regional west-east, dip-oriented cross section AA′ of the central part of the study area. Tkc, Tcl, Tmarm, and Tosw identify tops of Kansas City Formation, Cleveland formation, Marmaton Group, and Oswego limestone, respectively; other abbreviations are defined in the Figure 8 caption.
Image
—Regional north-south, strike-oriented cross section BB′ of the east-centra...
Published: 01 April 1994
Figure 9 —Regional north-south, strike-oriented cross section BB′ of the east-central part of the study area. Tkc, Tcl, Tmarm, and Tosw identify tops of Kansas City Formation, Cleveland formation, Marmaton Group, and Oswego limestone, respectively; other abbreviations are defined in the Figure 8
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1934
AAPG Bulletin (1934) 18 (2): 251–262.
... - A. The Oswego limestone is used as a datum bed and the section shows the attitude of the lower beds at the time the Oswego was deposited horizontally. At the beginning of Pennsylvanian deposition, the fold was well developed and the fault had a vertical displacement of about 2,000 feet, with an eastward facing...
FIGURES | View All (10)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1994
AAPG Bulletin (1994) 78 (4): 569–595.
...Figure 2 —Representative shelf-to-basin cross section of the Oswego limestone, Marmaton Group (undivided), Cleveland formation, and Kansas City Formation. Regional lithostratigraphic and sequence stratigraphic correlations presented in this report emphasize the dominantly siliciclastic section...
FIGURES | View All (18)
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1930
AAPG Bulletin (1930) 14 (12): 1515–1533.
...FIG. 6. —Subsurface maps on Oswego limestone and Arbuckle limestone. Contours on Oswego are on base of member. ...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1926
AAPG Bulletin (1926) 10 (2): 199.
... of Petroleum Geologists All evidence indicates that this cherty zone is the Fort Scott (“Oswego”) limestone member of the Marmaton formation. It is not at all uncommon to find chert in this member along its outcrop in Kansas and Missouri. 2 The sample obtained at a depth of 3,500 feet in this cherty...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1956
AAPG Bulletin (1956) 40 (1): 122–139.
... importance to this paper are the Checkerboard limestone at 3,800 feet, the Oswego limestone at 4,100 feet, and the Inola limestone at 4,400 feet. (The writer uses Frost’s [1940, p. 1997] designation of Inola, although he believes that it is actually the Pink limestone and has so shown on his correlated...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1948
AAPG Bulletin (1948) 32 (11): 2160.
...-paleogeographic activities; they are formed by Bald Eagle-Oswego-Juniata-Queenston sediments; the Shawangunk-Tuscarora-Medina-Clinton-McKenzie sediments; the Bloomsburg-Vernon-Wills Creek-Camillus sediments. Carbonates are significant in the McKenzie limestone and shale and Lockport dolomite above the Clinton...