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dc.contributor.advisorMazzullo, S. J.en_US
dc.contributor.authorTurner, Robert W.en_US
dc.date.accessioned2011-07-15T14:52:06Z
dc.date.available2011-07-15T14:52:06Z
dc.date.issued2011-05-04en_US
dc.identifier.citationTurner, Robert W. (2011). Cave-Fill Deposits in Pre-Atokan Paleocaves in the Mississippian (Osagean) Burlington-Keokuk Limestone in Southwestern Missouri. -- In Proceedings: 7th Annual Symposium: Graduate Research and Scholarly Projects. Wichita, KS: Wichita State University, p. 150-151en_US
dc.identifier.urihttp://hdl.handle.net/10057/3580
dc.descriptionPaper presented to the 7th Annual Symposium on Graduate Research and Scholarly Projects (GRASP) held at the Marcus Welcome Center, Wichita State University, May 4, 2011.en_US
dc.descriptionResearch completed at the Department of Geologyen_US
dc.description.abstractTwo siliciclastic-filled (sandstone and shale) paleocaves in the Mississippian (Osagean) Burlington-Keokuk Limestone are exposed in roadcuts in Dade County, Missouri. These caves formed in pre-Atokan time as suggested by their shale and/or sandstone fill, which contains Late Atokan spore and pollen fossil assemblages. These flora, and sedimentologic analysis, suggest that the cave-fill deposits were derived from Late Atokan terrestrial deposits (McLouth Formation) and not Desmoinesian age rocks (Krebs Group) that are exposed nearby. The McLouth Fm. similarly fills subsurface paleocaves in Leavenworth and Jefferson counties in Kansas.en_US
dc.language.isoen_USen_US
dc.publisherWichita State University. Graduate Schoolen_US
dc.relation.ispartofseriesGRASPen_US
dc.relation.ispartofseriesv.7en_US
dc.titleCave-Fill Deposits in Pre-Atokan Paleocaves in the Mississippian (Osagean) Burlington-Keokuk Limestone in Southwestern Missourien_US
dc.typeConference paperen_US


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