Difference between revisions of "Greenbush Coal Member"

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{{DISPLAYTITLE:Greenbush Coal Member or Bed}}
 
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|category4=Kewanee Group
 
|category4=Kewanee Group
 
|category5=Desmoinesian Series
 
|category5=Desmoinesian Series
|category6=Spoon Formation
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|category6=Carbondale Formation
 
|category7=Coal
 
|category7=Coal
 
|tree1=Kewanee Group
 
|tree1=Kewanee Group
|tree2=Spoon Formation
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|tree2=Carbondale Formation
 
|tree3=Greenbush Coal Member
 
|tree3=Greenbush Coal Member
 
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==Primary source==
 
==Primary source==
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.
+
Nelson, W.J., 2020, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey Bulletin (in press). <br>
 +
Edited and figures drafted by Jennifer M. Obrad.
  
 
==Contributing author&#40;s&#41;==
 
==Contributing author&#40;s&#41;==
M. E. Hopkins and J. A. Simon
+
W.J. Nelson
  
 
==Name==
 
==Name==
  
 
===Original description===
 
===Original description===
The Greenbush Coal Member of the Spoon Formation (Wanless, 1931a, p. 191).
+
Wanless (1931, p. 191) named the “Greenbush cyclical formation” and “Greenbush coal” together with the older Wiley cyclical formation and coal. Kosanke et al. (1960) formally designated it the Greenbush Coal Member (of the Spoon Formation).  
  
 
===Derivation===
 
===Derivation===
Named for Greenbush Township, Warren County.
+
The name refers to Greenbush Township in Warren County, Illinois.  
  
 
===Other names===
 
===Other names===
 +
None.
  
 
===History&#47;background===
 
===History&#47;background===
 +
None.
  
 
==Type section==
 
==Type section==
  
 
===Type location===
 
===Type location===
The type locality is in Greenbush Township (E 1/2 24, 8N-1W) (Wanless, 1956, p. 10; 1957, p. 81, 205).
+
The stratotype is a ravine tributary to Swan Creek in the E½ of sec. 24, T 8 N, R 1 W, in Warren County.  
  
 
===Type author&#40;s&#41;===
 
===Type author&#40;s&#41;===
 +
Wanless (1957, p. 81, 205).
  
 
===Type status===
 
===Type status===
 +
Unknown.
  
 
==Reference section==
 
==Reference section==
 +
[[file:Penn_carbondale_4-9.jpg|250px|{{file:Penn_carbondale_4-9.jpg}}|thumb]]
 +
None has been proposed, but Wanless (1957) described several outcrop sections that might suffice. A generalized section from the area Wanless mapped in western Illinois is presented here (Figure 4-9).
  
===Reference location===
+
==Stratigraphic relationships==
 
+
Wanless (1939) correlated the Greenbush with the Dekoven; Wanless (1956, 1957, 1962), Kosanke et al. (1960), and Willman et al. (1975) endorsed this correlation. Greenbush and Dekoven both occupy the second sedimentary cycle underlying the Colchester Coal (Figure 4-9). Fossil spore floras confirm the matchup of the Dekoven and Greenbush (Kosanke 1950; Peppers 1970, 1996).<br>
===Reference author&#40;s&#41;===
 
 
 
===Reference status===
 
  
==Stratigraphic relationships==
+
[[file:Penn_carbondale_4-12.jpg|250px|{{file:Penn_carbondale_4-12.jpg}}|left|thumb]]
 +
The name “Greenbush” would be ripe for abandonment on the basis of redundancy were it not for the fact that the type Dekoven Coal is now known to comprise the merger of two seams. The upper of these is the Abingdon; the lower lacks a name. Because Greenbush and Abingdon long have been known as separate units in western Illinois, it is a simple matter to extend the Greenbush into southern Illinois and western Kentucky as the lower “split” of the Dekoven Coal (Figure 4-12). Where the Greenbush is distinctly separate from the Davis and Abingdon, the Greenbush is classified as a member. The Greenbush becomes a bed where it merges with the Abingdon Coal to form the Dekoven Coal Member and where it merges with both Abingdon and Davis to become the Seelyville Coal Member.
  
 
==Extent and thickness==
 
==Extent and thickness==
The Greenbush Coal is seldom more than a few inches thick, and it grades into a thin carbonaceous shale in some localities.
+
Wanless (1957, p. 82) noted that “Not more than one or two inches [≤5 cm] of Greenbush coal has been found in western Illinois.” In southeastern Illinois, Jacobson (1993) stated that the “lower split of the Dekoven” [Greenbush] is normally 1 to 2 ft (30 to 60 cm) thick but locally reaches 3 ft (90 cm).  
  
 
==Lithology==
 
==Lithology==
 +
In western Illinois, where it is very thin, the Greenbush is shaly coal or carbonaceous shale. The thicker Greenbush (lower Dekoven) of southeastern Illinois is bright-banded coal having a moderate sulfur content and no consistent clastic layers.
  
 
==Core&#40;s&#41;==
 
==Core&#40;s&#41;==
Line 63: Line 70:
  
 
==Contacts==
 
==Contacts==
 +
Both contacts are sharp or rapidly gradational.
  
 
==Well log characteristics==
 
==Well log characteristics==
 +
Typical for coal.
  
 
==Fossils==
 
==Fossils==
 +
Kosanke (1950) and Peppers (1970, 1996) compared fossil spores of the Greenbush from western Illinois and the Dekoven Coal of southeastern Illinois and western Kentucky. The floras are closely similar, supporting the equivalence of the beds.
  
 
==Age and correlation==
 
==Age and correlation==
It is correlated with the De Koven Coal of southern Illinois and western Kentucky.
+
The Greenbush is likely to be equivalent to the Robinson Branch Coal Bed of Missouri and Kansas (Figure 4-12). There is no named correlative in Iowa or the Appalachian Basin.  
  
 
==Environments of deposition==
 
==Environments of deposition==
 +
The Western Shelf was a positive area, barely conducive to the formation and preservation of peat. More rapid tectonic subsidence in the deeper part of the basin allowed accumulation of coal in economic thickness.
  
 
==Economic importance==
 
==Economic importance==
 +
See the [[Dekoven Coal Member|Dekoven Coal]] and [[Seelyville Coal Member|Seelyville Coal]] Members.
  
 
==Remarks==
 
==Remarks==
  
 
==References==
 
==References==
WANLESS, H. R., 1931a, Pennsylvanian cycles in western Illinois: Illinois State Geological Survey Bulletin 60, p. <br>
+
*Jacobson, R.J., 1993, Coal resources of the Dekoven and Davis Members (Carbondale Formation) in Gallatin and Saline Counties, southeastern Illinois: Illinois State Geological Survey, Circular 551, 41 p., 5 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>
+
*Kosanke, R.M., 1950, Pennsylvanian spores of Illinois and their use in correlation: Illinois State Geological Survey, Bulletin 74, 128 p., 2 pls.<br>
WANLESS, H. R., 1957, Geology and mineral resources of the Beardstown, Glasford, Havana, and Vermont Quadrangles: Illinois State Geological Survey Bulletin 82, 233 p.<br>
+
*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. and 1 pl.<br>
 +
*Peppers, R.A., 1970, Correlation and palynology of coals in the Carbondale and Spoon Formations (Pennsylvanian) of the northeastern part of the Illinois Basin: Illinois State Geological Survey, Bulletin 93, 173 p.<br>
 +
*Peppers, R.A., 1996, Palynological correlation of major Pennsylvanian (Middle and Upper Carboniferous) chronostratigraphic boundaries in the Illinois and other coal basins: Geological Society of America, Memoir 188, 111 p. and correlation chart.<br>
 +
*Wanless, H.R., 1931, Pennsylvanian cycles in western Illinois: Illinois State Geological Survey, Bulletin 60, p. 179–193.<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>
 +
*Wanless, H.R., 1956, Classification of the Pennsylvanian rocks of Illinois as of 1956: Illinois State Geological Survey, Circular 217, 14 p.<br>
 +
*Wanless, H.R., 1957, Geology and mineral resources of the Beardstown, Glasford, Havana, and Vermont Quadrangles: Illinois State Geological Survey, Bulletin 82, 233 p.<br>
 +
*Wanless, H.R., 1962, Pennsylvanian rocks of Eastern Interior Basin, in C.C. Branson, ed., Pennsylvanian System in the United States, a symposium: Tulsa, Oklahoma, American Association of Petroleum Geologists, p. 4–59.<br>
 +
*Willman, H.B., E. Atherton, T.C. Buschbach, C. Collinson, J.C. Frye, M.E. Hopkins, J.A. Lineback, and J.A. Simon, 1975, Handbook of Illinois stratigraphy: Illinois State Geological Survey, Bulletin 95, 261 p.<br>
  
 
{{Codes
 
{{Codes

Revision as of 21:21, 2 February 2021

Lithostratigraphy: Kewanee Group >>Carbondale Formation >>Greenbush Coal Member
Chronostratigraphy: Paleozoic Erathem >>Pennsylvanian Subsystem >>Desmoinesian Series
Allostratigraphy: Absaroka Sequence

Primary source

Nelson, W.J., 2020, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey Bulletin (in press).
Edited and figures drafted by Jennifer M. Obrad.

Contributing author(s)

W.J. Nelson

Name

Original description

Wanless (1931, p. 191) named the “Greenbush cyclical formation” and “Greenbush coal” together with the older Wiley cyclical formation and coal. Kosanke et al. (1960) formally designated it the Greenbush Coal Member (of the Spoon Formation).

Derivation

The name refers to Greenbush Township in Warren County, Illinois.

Other names

None.

History/background

None.

Type section

Type location

The stratotype is a ravine tributary to Swan Creek in the E½ of sec. 24, T 8 N, R 1 W, in Warren County.

Type author(s)

Wanless (1957, p. 81, 205).

Type status

Unknown.

Reference section

Figure 4-9. Composite section for west-central Illinois. After Wanless (1957), with current names and correlations to Indiana, Kentucky, and southern Illinois. © University of Illinois Board of Trustees.

None has been proposed, but Wanless (1957) described several outcrop sections that might suffice. A generalized section from the area Wanless mapped in western Illinois is presented here (Figure 4-9).

Stratigraphic relationships

Wanless (1939) correlated the Greenbush with the Dekoven; Wanless (1956, 1957, 1962), Kosanke et al. (1960), and Willman et al. (1975) endorsed this correlation. Greenbush and Dekoven both occupy the second sedimentary cycle underlying the Colchester Coal (Figure 4-9). Fossil spore floras confirm the matchup of the Dekoven and Greenbush (Kosanke 1950; Peppers 1970, 1996).

Figure 4-12. Correlation of the Seelyville Coal Member and associated strata from Illinois to the Midcontinent Basin. Midcontinent data from Gentile and Thompson (2004), Pope (2012), Heckel (2013), and P.H. Heckel (personal communication, Aug. 1, 2014). Not to scale. © University of Illinois Board of Trustees.

The name “Greenbush” would be ripe for abandonment on the basis of redundancy were it not for the fact that the type Dekoven Coal is now known to comprise the merger of two seams. The upper of these is the Abingdon; the lower lacks a name. Because Greenbush and Abingdon long have been known as separate units in western Illinois, it is a simple matter to extend the Greenbush into southern Illinois and western Kentucky as the lower “split” of the Dekoven Coal (Figure 4-12). Where the Greenbush is distinctly separate from the Davis and Abingdon, the Greenbush is classified as a member. The Greenbush becomes a bed where it merges with the Abingdon Coal to form the Dekoven Coal Member and where it merges with both Abingdon and Davis to become the Seelyville Coal Member.

Extent and thickness

Wanless (1957, p. 82) noted that “Not more than one or two inches [≤5 cm] of Greenbush coal has been found in western Illinois.” In southeastern Illinois, Jacobson (1993) stated that the “lower split of the Dekoven” [Greenbush] is normally 1 to 2 ft (30 to 60 cm) thick but locally reaches 3 ft (90 cm).

Lithology

In western Illinois, where it is very thin, the Greenbush is shaly coal or carbonaceous shale. The thicker Greenbush (lower Dekoven) of southeastern Illinois is bright-banded coal having a moderate sulfur content and no consistent clastic layers.

Core(s)

Photograph(s)

Contacts

Both contacts are sharp or rapidly gradational.

Well log characteristics

Typical for coal.

Fossils

Kosanke (1950) and Peppers (1970, 1996) compared fossil spores of the Greenbush from western Illinois and the Dekoven Coal of southeastern Illinois and western Kentucky. The floras are closely similar, supporting the equivalence of the beds.

Age and correlation

The Greenbush is likely to be equivalent to the Robinson Branch Coal Bed of Missouri and Kansas (Figure 4-12). There is no named correlative in Iowa or the Appalachian Basin.

Environments of deposition

The Western Shelf was a positive area, barely conducive to the formation and preservation of peat. More rapid tectonic subsidence in the deeper part of the basin allowed accumulation of coal in economic thickness.

Economic importance

See the Dekoven Coal and Seelyville Coal Members.

Remarks

References

  • Jacobson, R.J., 1993, Coal resources of the Dekoven and Davis Members (Carbondale Formation) in Gallatin and Saline Counties, southeastern Illinois: Illinois State Geological Survey, Circular 551, 41 p., 5 pls.
  • Kosanke, R.M., 1950, Pennsylvanian spores of Illinois and their use in correlation: Illinois State Geological Survey, Bulletin 74, 128 p., 2 pls.
  • 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. and 1 pl.
  • Peppers, R.A., 1970, Correlation and palynology of coals in the Carbondale and Spoon Formations (Pennsylvanian) of the northeastern part of the Illinois Basin: Illinois State Geological Survey, Bulletin 93, 173 p.
  • Peppers, R.A., 1996, Palynological correlation of major Pennsylvanian (Middle and Upper Carboniferous) chronostratigraphic boundaries in the Illinois and other coal basins: Geological Society of America, Memoir 188, 111 p. and correlation chart.
  • Wanless, H.R., 1931, Pennsylvanian cycles in western Illinois: Illinois State Geological Survey, Bulletin 60, p. 179–193.
  • Wanless, H.R., 1939, Pennsylvanian correlations in the Eastern Interior and Appalachian coal fields: Geological Society of America, Special Paper 17, 130 p.
  • Wanless, H.R., 1956, Classification of the Pennsylvanian rocks of Illinois as of 1956: Illinois State Geological Survey, Circular 217, 14 p.
  • Wanless, H.R., 1957, Geology and mineral resources of the Beardstown, Glasford, Havana, and Vermont Quadrangles: Illinois State Geological Survey, Bulletin 82, 233 p.
  • Wanless, H.R., 1962, Pennsylvanian rocks of Eastern Interior Basin, in C.C. Branson, ed., Pennsylvanian System in the United States, a symposium: Tulsa, Oklahoma, American Association of Petroleum Geologists, p. 4–59.
  • Willman, H.B., E. Atherton, T.C. Buschbach, C. Collinson, J.C. Frye, M.E. Hopkins, J.A. Lineback, and J.A. Simon, 1975, Handbook of Illinois stratigraphy: Illinois State Geological Survey, Bulletin 95, 261 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation
3200
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