Drury Shale Member: Difference between revisions

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{{DISPLAYTITLE:Drury Shale Member (abandoned)}}
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{{Tree
{{Tree
|category1=Paleozoic Erathem
|category1=Abandoned Names
|category2=Pennsylvanian Subsystem
|category3=Absaroka Sequence
|category4=McCormick Group
|category5=Morrowan Series
|category6=Caseyville Formation
|category7=Shale
|tree1=McCormick Group
|tree1=McCormick Group
|tree2=Caseyville Formation
|tree2=Caseyville Formation
Line 16: Line 11:
|tree31=Absaroka Sequence
|tree31=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).
Willman, H. B., Elwood Atherton, T. C. Buschbach, Charles Collinson, John C. Frye, M. E. Hopkins, Jerry A. Lineback, and Jack A. Simon, 1975, Handbook of Illinois Stratigraphy: Illinois State Geological Survey Bulletin 95, 261 p.


==Contributing author(s)==
==Contributing author(s)==
M. E. Hopkins and J. A. Simon
W.J. Nelson


==Name==
==Name==


===Original description===
===Original description===
The Drury Shale Member of the Caseyville Formation (Lamar, 1925, p. 91-95).
Lamar (1925, p. 91–95) divided the Pottsville Formation into four newly named members in the Carbondale, Illinois, 15-minute quadrangle. In ascending order, these were the Wayside sandstone and shale, the Lick Creek sandstone, the Drury sandstone and shale, and the Makanda sandstone. Among the four, only the name Wayside is still in use.


===Derivation===
===Derivation===
Named for Drury Creek in Jackson County.
The unit took its name from Drury Creek, a north-flowing tributary of the Big Muddy River in Union and Jackson Counties, southern Illinois.


===Other names===
===Other names===
None.


===History/background===
===History/background===
[[file:Penn_caseyville_2-7.jpg|250px|{{file:Penn_caseyville_2-7.jpg}}|thumb]]
With the rise of cyclic classification, the Drury became a formation in the Caseyville Group (Wanless 1939). However, Weller (1940) and Wanless (1956) showed it as the Drury shale member of the Battery Rock formation. Kosanke et al. (1960) formalized the unit as the Drury Shale Member of the Caseyville Formation (Figure 2-7).<br>
Remapping the southeastern part of the Carbondale 15-minute quadrangle, Nelson and Weibel (1996, p. 21) determined that the Drury Member, as mapped by Lamar (1925), “is largely in the lower part of the Tradewater Formation, although in some areas the Drury includes uppermost Caseyville strata.” Lamar’s original usage of Drury therefore conflicted with later usage, which placed the Drury entirely within the Caseyville. Rather than redefining the Drury, Nelson and Weibel opted to leave the interval unnamed. Additional factors favoring abandonment include extreme lithologic variability of the Drury and inability to demarcate the member in areas where either the [[Pounds Sandstone Member|Pounds]] or [[Battery Rock Sandstone Member|Battery Rock]] Sandstones cannot be identified.<br>


==Type section==
==Type section==
 
None was designated or described.
===Type location===
The type section consists of exposures along Drury Creek south of Makanda (33, 34, 10S-1W).
 
===Type author&#40;s&#41;===
 
===Type status===
 
==Reference section==
 
===Reference location===
 
===Reference author&#40;s&#41;===
 
===Reference status===
 
==Stratigraphic relationships==
All strata lying between the Battery Rock and Pounds Sandstones are considered equivalent to the Drury, but, for the sake of clarity in classification, the name "Drury" is not used in parts of southeastern Illinois where two other members of the Caseyville Formation - the Sellers Limestone and the Gentry Coal - occur within the Drury interval.
 
==Extent and thickness==
The Drury is as much as 100-150 feet thick in places near the type area, but the thickness varies somewhat, partly because of differential erosion prior to deposition of the overlying Pounds Sandstone.
 
==Lithology==
The Drury is a complex unit of sandy or silty shale, siltstone, and lenticular massive sandstone units, and is much like the Lusk Shale. It contains at least two thin, nonpersistent coals. Although rocks of Drury age are present in the subsurface of the southern part of the Illinois Basin, the Battery Rock and Pounds Sandstones cannot generally be differentiated in well logs, which makes it impractical to differentiate the Drury.
 
==Core&#40;s&#41;==
 
==Photograph&#40;s&#41;==
 
==Contacts==
 
==Well log characteristics==
 
==Fossils==
 
==Age and correlation==
The Drury is equivalent to part of the Mansfield Sandstone of Indiana.
 
==Environments of deposition==
 
==Economic importance==
 
==Remarks==


==References==
==References==
LAMAR, J. E., 1925, Geology and mineral resources of the Carbondale Quadrangle: Illinois State Geological Survey Bulletin 48, 172 p.
* Kosanke, R.M., J.A. Simon, H.R. Wanless, and H.B. Willman, 1960, Classification of the Pennsylvanian strata of Illinois: Illinois State Geological Survey, Report of Investigations 214, 84 p., 1 pl.<br>
* Lamar, J.E., 1925, Geology and mineral resources of the Carbondale Quadrangle: Illinois State Geological Survey, Bulletin 48, 173 p., 3 pls.<br>
* Nelson, W.J., and C.P. Weibel, 1996, Geology of the Lick Creek Quadrangle, Johnson, Union, and Williamson Counties, southern Illinois: Illinois State Geological Survey, Bulletin 103, 39 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., 9 pls.<br>
* Wanless, H.R., 1956, Classification of the Pennsylvanian rocks of Illinois as of 1956: Illinois State Geological Survey, Circular 217, 14 p.<br>
* Weller, J.M., 1940, Geology and oil possibilities of extreme southern Illinois: Illinois State Geological Survey, Report of Investigations 71, 71 p.<br>


{{Codes
{{Codes

Latest revision as of 16:32, 9 February 2022

Lithostratigraphy: McCormick Group >>Caseyville Formation >>Drury Shale Member
Chronostratigraphy: Paleozoic Erathem >>Pennsylvanian Subsystem >>Morrowan Series
Allostratigraphy: Absaroka Sequence

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

Lamar (1925, p. 91–95) divided the Pottsville Formation into four newly named members in the Carbondale, Illinois, 15-minute quadrangle. In ascending order, these were the Wayside sandstone and shale, the Lick Creek sandstone, the Drury sandstone and shale, and the Makanda sandstone. Among the four, only the name Wayside is still in use.

Derivation

The unit took its name from Drury Creek, a north-flowing tributary of the Big Muddy River in Union and Jackson Counties, southern Illinois.

Other names

None.

History/background

Figure 2-7. Chart showing the history of usage of the Drury Member. © University of Illinois Board of Trustees.

With the rise of cyclic classification, the Drury became a formation in the Caseyville Group (Wanless 1939). However, Weller (1940) and Wanless (1956) showed it as the Drury shale member of the Battery Rock formation. Kosanke et al. (1960) formalized the unit as the Drury Shale Member of the Caseyville Formation (Figure 2-7).

Remapping the southeastern part of the Carbondale 15-minute quadrangle, Nelson and Weibel (1996, p. 21) determined that the Drury Member, as mapped by Lamar (1925), “is largely in the lower part of the Tradewater Formation, although in some areas the Drury includes uppermost Caseyville strata.” Lamar’s original usage of Drury therefore conflicted with later usage, which placed the Drury entirely within the Caseyville. Rather than redefining the Drury, Nelson and Weibel opted to leave the interval unnamed. Additional factors favoring abandonment include extreme lithologic variability of the Drury and inability to demarcate the member in areas where either the Pounds or Battery Rock Sandstones cannot be identified.

Type section

None was designated or described.

References

  • Kosanke, R.M., J.A. Simon, H.R. Wanless, and H.B. Willman, 1960, Classification of the Pennsylvanian strata of Illinois: Illinois State Geological Survey, Report of Investigations 214, 84 p., 1 pl.
  • Lamar, J.E., 1925, Geology and mineral resources of the Carbondale Quadrangle: Illinois State Geological Survey, Bulletin 48, 173 p., 3 pls.
  • Nelson, W.J., and C.P. Weibel, 1996, Geology of the Lick Creek Quadrangle, Johnson, Union, and Williamson Counties, southern Illinois: Illinois State Geological Survey, Bulletin 103, 39 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., 9 pls.
  • Wanless, H.R., 1956, Classification of the Pennsylvanian rocks of Illinois as of 1956: Illinois State Geological Survey, Circular 217, 14 p.
  • Weller, J.M., 1940, Geology and oil possibilities of extreme southern Illinois: Illinois State Geological Survey, Report of Investigations 71, 71 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation
3890
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