Spickert Knob Formation (New), Borden Group, in Indiana

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dc.contributor.authorRexroad, Carl Buckner
dc.contributor.authorLane, Norman Gary
dc.date.accessioned2022-09-12T17:11:37Z
dc.date.available2022-09-12T17:11:37Z
dc.date.issued1984
dc.description.abstractAlthough stratigraphic nomenclature within the Borden Group of early Valmeyeran age has remained stable in Indiana since Stockdale's (1929,1931) definitive studies, recognition of the boundary between the Locust Point Formation and the overlying Carwood Formation has not been practicable outside the type area of the Borden and its subdivisions in Harrison, Floyd, and Clark Counties. The Locust Point and the Carwood form a depositional unit of delta-slope sediments in the middle part of the Borden deltaic sequence. They overlie the prodelta sediments of the New Providence Shale and underlie the delta-platform sequence of the Edwardsville Formation.en
dc.identifier.citationRexroad, C. B., and Lane, N. G., 1984, Spickert Knob Formation (new), Borden Group, in Indiana: Indiana Department of Conservation Geological Survey Occasional Paper 43, 10 p.en
dc.identifier.urihttps://hdl.handle.net/2022/28168
dc.language.isoenen
dc.publisherIndiana Department of Conservation Geological Surveyen
dc.relation.ispartofseriesOccasional Papers;43
dc.rightsThis work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 4.0 License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/4.0/ or send a letter to Creative Commons, 543 Howard Street, 5th Floor, San Francisco, California, 94105, USA.en
dc.rights.urihttps://creativecommons.org/licenses/by-sa/4.0/en
dc.subjectStratigraphyen
dc.subjectSpickert Knob Formationen
dc.titleSpickert Knob Formation (New), Borden Group, in Indianaen
dc.typeTechnical Reporten

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