Sebree Sandstone Member: Difference between revisions

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{{DISPLAYTITLE:Sebree Sandstone Member (abandoned)}}
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{{Tree
{{Tree
|category1=Paleozoic Erathem
|category1=Abandoned Names
|category2=Pennsylvanian Subsystem
|tree1=Carbondale Formation
|category3=Absaroka Sequence
|tree2=Sebree Sandstone Member
|category4=Kewanee Group
|category5=Desmoinesian Series
|category6=Carbondale Formation
|category7=Sandstone
|tree1=Kewanee Group
|tree2=Carbondale Formation
|tree21=Paleozoic Erathem
|tree21=Paleozoic Erathem
|tree22=Pennsylvanian Subsystem
|tree22=Pennsylvanian Subsystem
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==Primary source==
==Primary source==
Nelson, W.J., 2020, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey Bulletin (in press). <br>
Nelson, W.J., P.H. Heckel and J.M. Obrad, 2022, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey, Bulletin (in press).
Edited and figures drafted by Jennifer M. Obrad.


==Contributing author&#40;s&#41;==
==Contributing author&#40;s&#41;==
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===Original description===
===Original description===
Greb et al. (1992) attributed the Sebree Sandstone to Glenn (1912), but no reference to this unit appears therein. The earliest known reference to the Sebree Sandstone appears in Glenn (1922, p. 97–98).


===Derivation===
===Derivation===
Sebree is a community of about 1,500 people in northeastern Webster County, Kentucky.


===Other names===
===Other names===
 
None.
===History&#47;background===


==Type section==
==Type section==


===Type location===
===Type location===
No specific locality was designated. Glenn (1922, p. 97–98) described the Sebree as coarse, cross-bedded sandstone that forms ridges and cliffs near Sebree and Steamport Landing in eastern Webster County, Kentucky.


===Type author&#40;s&#41;===
===Type author&#40;s&#41;===
Glenn (1922, p. 97–98).


===Type status===
===Type status===
Unknown.


==Reference section==
==Reference section==
 
None.
===Reference location===
 
===Reference author&#40;s&#41;===
 
===Reference status===


==Stratigraphic relationships==
==Stratigraphic relationships==
 
Plate 31 in Glenn (1922) shows the unit to be 15 to 65 ft (4.5 to 20 m) thick and to lie between the Nos. 7 and 8 coal beds (Dekoven and Survant). Wanless (1939) refined the position of the Sebree Sandstone to be between the Colchester and Dekoven coal beds, which is the same position as that of the earlier named [[Coxville Sandstone Member|Coxville Sandstone]]. The name Sebree Sandstone is hereby abandoned in favor of [[Coxville Sandstone Member|Coxville Sandstone]] on the basis of priority.
==Extent and thickness==
 
==Lithology==
 
==Core&#40;s&#41;==
 
==Photograph&#40;s&#41;==
 
==Contacts==
 
==Well log characteristics==
 
==Fossils==
 
==Age and correlation==
 
==Environments of deposition==
 
==Economic importance==
 
==Remarks==


==References==
==References==
*Glenn, L.C., 1912, A geological reconnaissance of the Tradewater River region, with special reference to the coal beds: Kentucky Geological Survey, Bulletin 17, 75 p.<br>
*Glenn, L.C., 1922, The geology and coals of Webster County, Kentucky: Kentucky Geological Survey, Series 6, v. 5, 249 p.<br>
*Greb, S.F., D.A. Williams, and A.D. Williamson, 1992, Geology and stratigraphy of the western Kentucky coal field: Kentucky Geological Survey, Series 11, Bulletin 2, 77 p., 1 pl.<br>
*Wanless, H.R., 1939, Pennsylvanian correlations in the Eastern Interior and Appalachian coal fields: Geological Society of America, Special Paper 17, 130 p.<br>


{{Codes
{{Codes
|membercode=0000
|membercode=--
|geo_unit=--
|geo_unit=--
}}
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Latest revision as of 16:35, 9 February 2022

Lithostratigraphy: Carbondale Formation >>Sebree Sandstone Member
Chronostratigraphy: Paleozoic Erathem >>Pennsylvanian Subsystem >>Desmoinesian Series
Allostratigraphy: Absaroka Sequence

Primary source

Nelson, W.J., P.H. Heckel and J.M. Obrad, 2022, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey, Bulletin (in press).

Contributing author(s)

W.J. Nelson

Name

Original description

Greb et al. (1992) attributed the Sebree Sandstone to Glenn (1912), but no reference to this unit appears therein. The earliest known reference to the Sebree Sandstone appears in Glenn (1922, p. 97–98).

Derivation

Sebree is a community of about 1,500 people in northeastern Webster County, Kentucky.

Other names

None.

Type section

Type location

No specific locality was designated. Glenn (1922, p. 97–98) described the Sebree as coarse, cross-bedded sandstone that forms ridges and cliffs near Sebree and Steamport Landing in eastern Webster County, Kentucky.

Type author(s)

Glenn (1922, p. 97–98).

Type status

Unknown.

Reference section

None.

Stratigraphic relationships

Plate 31 in Glenn (1922) shows the unit to be 15 to 65 ft (4.5 to 20 m) thick and to lie between the Nos. 7 and 8 coal beds (Dekoven and Survant). Wanless (1939) refined the position of the Sebree Sandstone to be between the Colchester and Dekoven coal beds, which is the same position as that of the earlier named Coxville Sandstone. The name Sebree Sandstone is hereby abandoned in favor of Coxville Sandstone on the basis of priority.

References

  • Glenn, L.C., 1912, A geological reconnaissance of the Tradewater River region, with special reference to the coal beds: Kentucky Geological Survey, Bulletin 17, 75 p.
  • Glenn, L.C., 1922, The geology and coals of Webster County, Kentucky: Kentucky Geological Survey, Series 6, v. 5, 249 p.
  • Greb, S.F., D.A. Williams, and A.D. Williamson, 1992, Geology and stratigraphy of the western Kentucky coal field: Kentucky Geological Survey, Series 11, Bulletin 2, 77 p., 1 pl.
  • Wanless, H.R., 1939, Pennsylvanian correlations in the Eastern Interior and Appalachian coal fields: Geological Society of America, Special Paper 17, 130 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation
--
--

"--" is not a number.