Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Paleokarstic features and their relationship to cementation history, Burlington-Keokuk Limestone, middle Mississippian, central Missouri

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5378267
Various paleokarstic features, large scale to microscopic in size, are present in the upper Burlington-Keokuk Formation below the pre-Pennsylvanian unconformity in central Missouri. Solutional cavities of widely varying size and morphology are infilled with various sediment types including shale, peat, detrital quartz sand, residual chert, reworked limestone sediment and dolomite clasts, and pore-filling calcite cement. Wavy horizontal solution seams and solution-enlarged vertical fractures contain sandstone, shale, chert, and reworked limestone sediment. Chert nodules, apparently rotated from their original position, are commonly present in association with these features. The petrography of the paleokarstic features integrated with a regionally consistent luminescent zonal sequence in calcite cement provided new evidence for the timing of these cements. First-generation nonferroan cement predates the major period of karstification, whereas second-generation ferroan and third-generation calcite cement postdate the karstic event. Therefore, the karstification may have occurred while the limestone was relatively porous. Cement in cavity fills, host limestone, and overlying Pennsylvanian strata suggest karstification is post-Mississippian but no later than the Desmoinesian. A post-Desmoinesian age is indicated for second- and third-generation cements, previously believed to be Mississippian. The postkarstification timing for second-generation ferroan and third-generation calcite cement and the fact that they postdate a major regional compaction event suggest that they may have precipitated under burial conditions. Stratigraphic information constrains the amount of overburden as less than 1 km. Minor barite and sphalerite mineralization, believed to be Late Pennsylvanian or Early Permian, postdates calcite cementation and places a minimum age on the cement.
Research Organization:
State Univ. of New York, Stony Brook
OSTI ID:
5378267
Report Number(s):
CONF-860624-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 70:5
Country of Publication:
United States
Language:
English

Similar Records

Cement stratigragraphy of the Wahoo Formation, Sadlerochit Mountains, Alaska
Conference · Tue May 01 00:00:00 EDT 1990 · AAPG Bulletin (American Association of Petroleum Geologists); (USA) · OSTI ID:6720597

Diagenesis of the Lisburne Group, northeastern Brooks Range, Alaska
Technical Report · Mon May 01 00:00:00 EDT 1995 · OSTI ID:95603

Pre-Pennsylvanian paleokarst at the top of the upper Pennington Formation, central Tennessee
Conference · Mon Feb 28 23:00:00 EST 1994 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:6786548