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

Lithofacies variation across the Mammoth Cave-Pope Megagroup boundary -- a sequence stratigraphic approach

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:6837953
; ;  [1]
  1. Southern Illinois Univ., Carbondale, IL (United States). Dept. of Geology

Regional stratigraphic relations in southern Illinois suggest a major unconformity near the top of the St. Genevieve Limestone. Large exposures below the unconformity within the Anna quarries display a retrogradational parasequence-stacking pattern. Eight to 12 m-thick parasequences comprise thinning-upward marine bioclastic wackestone overlain by oolitic and bioclastic thickening-upward eolian( ) grainstone. An eolian origin for the bioclastic grainstones is supported by large scale cross stratification (0.5 to 2 m-thick sets), reworked character of rounded, coated bioclasts, and preserved duneforms. At the quarries, the unconformity is directly overlain by mudstones and sandstones. Thinning-upward mudstones interbedded with very thin (1 to 3 cm thick) intraclastic packstone tempestites crop out in a roadcut about 500 m NE of the quarries. Small-scale ripples and absence of trace fossils in lower mudstone units suggest an estuarine or lagoonal, brackish-waver environment. The trace fossil Conostichus and horizontal burrows appear abruptly in the upper, thin mudstone units. Highly bioturbated green and red shales overlying a 1 to 4 m-thick covered interval in a roadcut 610 m farther north are interbedded with tidally deposited, medium- to coarse-grained, bioclastic grainstones. The shale-draped, medium cross-bedded grainstones document ten or more tidal bundles. The cross-bedded grainstone is overlain by wavy- to flaser-bedded very fine-grained sandstone suggestive of sand flat origin. These sandstones are overlain by the Aux Vases Sandstone. Numerous low-angle bounding surfaces within the Aux Vases enclose low-angle, wedge-planar cross-bedding. A single irregular surface coated by a few centimeters of poorly sorted unstratified sandstone defines a ravinement surface near the base of the Aux Vases Sandstone.

OSTI ID:
6837953
Report Number(s):
CONF-9404217--
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Journal Name: Geological Society of America, Abstracts with Programs; (United States) Vol. 26:5; ISSN GAAPBC; ISSN 0016-7592
Country of Publication:
United States
Language:
English

Similar Records

Aux Vases-Renault-Yankeetown depositional sequence in comparison to other Chesterian depositonal sequences
Conference · Thu Sep 01 00:00:00 EDT 1983 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:6576916

Stratigraphic traps and deposition of Aux Vases and uppermost Ste. Geneieve Formations (Mississippian), Southern Illinois
Conference · Thu Sep 01 00:00:00 EDT 1983 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:6825014

Storm deposits (tempestites) in Ordovician cratonic carbonates (Arbuckle Group, south-central Oklahoma)
Conference · Mon Feb 28 23:00:00 EST 1983 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:6436765