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Contents

   



(Top)
 


1 Stratigraphy  



1.1  Kinkaid Formation  





1.2  Tobinsport Formation  





1.3  Degonia Formation  





1.4  Clore Formation  





1.5  Palestine Formation  





1.6  Menard Formation  





1.7  Waltersburg Formation  





1.8  Vienna Formation  





1.9  Tar Springs Formation  





1.10  Glen Dean Formation  





1.11  Hardinsburg Formation  





1.12  Haney Formation  





1.13  Fraileys Formation  





1.14  Beech Creek Formation  





1.15  Cypress Formation  





1.16  Ridenhower Formation  





1.17  Bethel Formation  







2 Energy Production  





3 References  














Pope Mega Group







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From Wikipedia, the free encyclopedia
 

(Redirected from Degonia Formation)

Pope Mega Group
Stratigraphic range: Carboniferous
TypeGeological group
Sub-units
  • Grove Church Shale
  • Kincaid
    • Goreville Limestone
    • Cave Hill Shale
    • Negli Creek Limestone
  • Degonia Sandstone
  • Clore Limestone
    • Ford Station Limestone
    • Tygett Sandstone
    • Cora Limestone
  • Palestine Sandstone
  • Menard Limestone
    • Allard Limestone
    • Scottsburg Limestone
    • Walche Limestone
  • Waltersburg Formation
  • Vienna Limestone
  • Tar Springs Sandstone
  • Glen Dean Formation
  • Hardinsburg Formation
  • Haney Formation
  • Fraileys Formation
    • Big Clifty Member
  • Beech Creek Formation
  • Cypress Formation
  • Ridenhower Formation
    • Reelsville Member
    • Sample Member
    • Beaver Bend Member
  • Bethel Formation
  • Downeys Bluff Formation
  • Yankeetown Formation
  • Renault Formation
    • Shellersville Member
    • Levias Member
  • Aux Vases Formation
OverliesMammoth Cave Group
Lithology
PrimarySandstone, Limestone, Shale
Location
RegionIllinois Basin
CountryUnited States of America

The Pope Mega Group is a geologic unit found in the Illinois Basin of southern Illinois, southwestern Indiana, and western Kentucky.[1][2]InIndiana and Kentucky its equitant is the Buffalo Wallow Group. This unit grades from sandstones at its base into mix of limestones and sandstone and then a shale at its top.[3] In Southern Illinois oil wells are drilled into the Tar Springs formation.[4]

Stratigraphy[edit]

Kinkaid Formation[edit]

Also known at the Kinkaid Limestone, this unit is made up of several smaller members. This unit ranges from 0' - 230 ' thick. The Grove Church Shale is at the top, followed by Members, Goreville Limestone, Cave Hill Shale, and Negli Creek Limestone.

Tobinsport Formation[edit]

A formation in Illinois containing 4 members that are linked to other formations in the Upper Pope Group. The Negli Creek Limestone of the Kinkaid formation to the west. Mt. Pleasant Sandstone, Bristow Sandstone, and Siberia Limestone. The Siberia is a thin tongue of the Menard formation.[5]

Degonia Formation[edit]

This sandstone unit is 0-150' thick.

Clore Formation[edit]

This unit is 0-150’ thick. Its units include the Ford Station Limestone, Tygett Sandstone and Cora Limestone Members.

Palestine Formation[edit]

This sandstone unit is 0-120' thick.

Menard Formation[edit]

The Menard Limestone is a geologic formation in the Illinois Basin of southern Illinois, southwestern Indiana, and western Kentucky.

The type section of both the Walche Limestone Member and the Scottsburg Limestone Member are exposures in Walche's Cut, a railway cutting on the Illinois Central Railroad.[6][7][8]

Waltersburg Formation[edit]

This formation is 0-100’ thick.

Vienna Formation[edit]

This limestone unit is 0-60' thick

Tar Springs Formation[edit]

This sandstone unit is 0-150' thick. The Tar Springs consists of interbedded sandstone and shale, creating closed reservoirs within the sand. For this reason it is the largest oil producing formation in Illinois. Estimated to have accounted for more than 60% of the oil production in the state.

Glen Dean Formation[edit]

The Glen Dean Formation is a geologic formationinIllinois, Indiana and Kentucky. It preserves fossils dating back to the Carboniferous period.

Hardinsburg Formation[edit]

The Hardinsburg Formation is a geologic formationinIllinois, Indiana and Kentucky. It preserves fossils dating back to the Carboniferous period.

Haney Formation[edit]

The Haney Formation is a geologic formationinIllinois, Indiana and Kentucky. It preserves fossils dating back to the Carboniferous period.

Fraileys Formation[edit]

The Fraileys FormationorFraileys Shale is a geologic formationinIllinois. It preserves fossils dating back to the Carboniferous period.

Beech Creek Formation[edit]

The Beech Creek Formation is a geologic formationinIllinois, Indiana and Kentucky. It preserves fossils dating back to the Carboniferous period.

Cypress Formation[edit]

The Cypress Formation is a geologic formationinIllinois, Indiana and Kentucky. It preserves fossils dating back to the Carboniferous period.

Ridenhower Formation[edit]

The Ridenhower Formation is a geologic formationinIllinois. It preserves fossils dating back to the Carboniferous period. It includes the Reelsville Member, Sample Member and Beaver Bend Member.

Bethel Formation[edit]

The Bethel Formation is a geologic formationinIllinois, Indiana and Kentucky. It preserves fossils dating back to the Carboniferous period.

Energy Production[edit]

References[edit]

  • ^ Willman, H.B., Atherton, Elwood, Buschbach, T.C., Collinson, Charles, Frye, J.C., Hopkins, M.E., Lineback, J.A., and Simon, J.A., 1975, Handbook of Illinois stratigraphy: Illinois Geological Survey Bulletin, no. 95, 261 p.
  • ^ Kolata, D.R. 2005, Bedrock Geology of Illinois: Champaign, Ill. U.S. Geological Survey (Report). Retrieved 16 December 2023.
  • ^ Askari, Zohreh; Lasemi, Yaghoob (16 December 2022). "Geological characterization and ROZ potential of the Tar Springs Sandstone". U.S. Department of Energy Office of Scientific and Technical Information.
  • ^ Gray, Henry H. (1978). Buffalo Wallow Group Upper Chesterian (Mississippian) of Southern Indiana (Report). Indiana Geological & Water Survey.
  • ^ "Walche Limestone Member". igws.indiana.edu.
  • ^ Swann, David Henry (November 17, 1963). "Classification of Genevievian and Chesterian (late Mississippian) rocks of Illinois". Report of Investigations No. 216 – via www.ideals.illinois.edu.
  • ^ Droste, J. B., and Keller, S. J., 1995, Subsurface stratigraphy and distribution of oil fields of the Buffalo Wallow Group (Mississippian) in Indiana: Indiana Geological Survey Bulletin 63, 24 p.


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    This page was last edited on 8 July 2024, at 13:04 (UTC).

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