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Keokuk beds

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Journal Article
Journal: Economic Geology
Published: 01 December 1966
Economic Geology (1966) 61 (8): 1436-1442.
... to 110 feet, in the vicinity of the Oronogo-Webb City-Duenweg field, than it was to the west near the Picher field where it was deposited in thicknesses of 70 to 80 feet. Post-Keokuk erosion has caused local removal of the top of the M bed in the western portion of the Picher field, and westward from...
Journal Article
Journal: Economic Geology
Published: 01 December 1965
Economic Geology (1965) 60 (8): 1607-1619.
... of southwestern Missouri, northeastern Oklahoma and southeastern Kansas and is a part of the Mississippian Keokuk Formation.One hundred and twenty specimens from this bed were collected under-ground from six pull drifts in five mines: West Side, Grace B, Big John, Little Greenback, and Mudd Mines. The specimens...
Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2008.2437(04)
... that breccia clasts in one polymict breccia contain a Middle Permian post-depositional magnetization in magnetite ( Elmore and Dulin, 2007 ). Eighteen sites (six to eight specimens per site) were sampled from tilted beds within the deformed Burlington-Keokuk Limestone in the Ash Grove Aggregates Quarry...
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Series: GSA Memoirs
Published: 01 March 1957
DOI: 10.1130/MEM67V2-p279
... being prominent. The Chouteau limestone is principally an argillaceous fine-grained limestone, but it also contains beds of medium crystalline limestone and some dolomitic limestone. It contains a large and varied fauna mainly of benthonic invertebrates. The Sedalia-Burlington-Keokuk limestone series...
Journal Article
Published: 01 January 1983
Journal of Paleontology (1983) 57 (1_Part_I): 112-123.
... environment stratigraphically above delta slope beds of the Cowbell Member of the Borden and is thus environmentally equivalent to the Edwardsville Formation of the Borden Group farther west in north-central Kentucky and southern Indiana. The Edwardsville is equivalent to the Keokuk Limestone of the standard...
Journal Article
Journal: GSA Bulletin
Published: 01 October 1948
GSA Bulletin (1948) 59 (10): 1027-1052.
... zone carries abundant crinoids, and higher zones correspond to the Burlington, Keokuk, Moorefield, and Chester. The Pennsylvanian limestones, 1600 feet thick, also contain a midwestern fauna. The Permian, 8500 feet thick, is divided into a lower, sandy, and essentially nonfossiliferous facies...
Journal Article
Published: 01 November 2013
Journal of Sedimentary Research (2013) 83 (11): 928-941.
...Cornelius M. Rott; Hairuo Qing A bstract : The Mississippian (Lower Carboniferous) Alida Beds of the northern Williston Basin, Canada, are carbonate rocks that contain a number of significant hydrocarbon reservoirs. These shallow marine carbonate platform deposits consist of abundant very finely...
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Journal Article
Published: 01 October 2006
Journal of Foraminiferal Research (2006) 36 (4): 379-388.
... Formation is of interest because in Keokuk County the Pella immediately overlies a fossil tetrapod deposit that is the oldest of its kind in North America. It sits above Romer’s Gap in the fossil record of early tetrapod evolution. Occurrences of the foraminifer Asteroarchaediscus rugosus indicate...
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Journal Article
Published: 01 November 2004
Journal of Paleontology (2004) 78 (6): 1128-1137.
... Providence Shale Member of the Borden Formation in north-central Kentucky. Both ammonoids and conodonts indicate an early late Osagean (lower Keokuk equivalent) age corresponding to the middle or, more probably, the late Chadian (latest Tournaisian or early Viséan) portion of the Fascipericyclus...
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Series: GSA Field Guide
Published: 01 January 2010
DOI: 10.1130/2010.0017(04)
EISBN: 9780813756172
... on the groundwater-table level). The Burlington-Keokuk is particularly noted for springs ( Vandike, 2001 , p. 53). In the setting around Wilson’s Creek Battlefield, chert beds or thin shale beds likely provided semi-permeable confining layers at the base of an unconfined aquifer. Springs played an important role...
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Journal Article
Published: 01 July 2007
Journal of Paleontology (2007) 81 (4): 737-745.
... burlingtonensis n. sp. and Richterella carteri n. sp. from the Burlington Formation of Missouri, Australosutura osagensis n. sp. from the Keokuk Limestone of Missouri and the Arcente and Dona Ana Members of the Lake Valley Formation of New Mexico, and Spergenaspis boonensis n. sp. from the Boone Formation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 2009
AAPG Bulletin (2009) 93 (12): 1649-1689.
...-continent. Cowley lithologies represent a low-gradient ramp, whereon (1) bedded spiculites were deposited in moderate-energy, shallow-water, inner-ramp settings; (2) lenticular-, nodular-, or flaser (L/N/F)-bedded spiculite and shale were moderate- to low-energy, progressively deeper-water medial-ramp...
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Journal Article
Published: 01 December 2003
Clays and Clay Minerals (2003) 51 (6): 675-688.
...O. Isik Ece; Zenbe-E Nakagawa; Paul A. Schroeder Abstract The Şile Region contains discontinuous, cyclic, thin coal beds and industrial clay deposits that were accumulated in lacustrine basins which received extensive volcanoclastic sediments due to transport of highly weathered calc-alkaline...
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Series: GSA Field Guide
Published: 01 January 2010
DOI: 10.1130/2010.0017(03)
EISBN: 9780813756172
... crinoidal grainstone with thick-to-massive bedding and widely spaced joints. Thus, the Burlington-Keokuk Formation is ideally suited for channeling of recharging water along discrete discontinuities, leading to the formation of karst and caves. Riverbluff Cave is just one of hundreds of caves in Greene...
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Journal Article
Published: 01 March 2011
Journal of Sedimentary Research (2011) 81 (3): 218-232.
... at the bed and formation scale, but did result in a general increase in pore size and an associated substantial increase in permeability compared to limestone precursors. Dolomitization differentially affects the porosity and permeability of carbonate strata on the scale of individual crystals, beds...
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Journal Article
Journal: Geology
Published: 01 March 2017
Geology (2017) 45 (3): 219-222.
... a lack of consensus as to how they form. In particular, multiple phases of diagenetic overprinting can obscure geochemical fingerprints. Study of a Cenozoic succession with a relatively simple burial history here provides new insights into the development of differentially dolomitized beds. The Hammam...
Journal Article
Journal: Economic Geology
Published: 01 March 2005
Economic Geology (2005) 100 (2): 295-309.
...D. T. A. Symons; S.J. Pannalal; R. M. Coveney, Jr.; D. F. Sangster Abstract Paleomagnetic results are reported from five Upper Mississippian and 19 Upper Pennsylvanian limestone and black shale sites (272 samples) and from 42 boulders, oriented with respect to their bedding, of Mississippi Valley...
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Journal Article
Published: 01 July 2014
Journal of Sedimentary Research (2014) 84 (7): 552-566.
...-Huqf High in central-east Oman. Mud-dominated peritidal carbonates rich in microbial mats are replaced by fine crystalline dolomite along at least 60 km in the lower 10 m of the Jurf Formation. Two, meter-thick beds in the overlying Qishn Formation are also dolomitized over lateral distances of one...
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Journal Article
Published: 01 November 2007
Journal of Sedimentary Research (2007) 77 (11): 939-964.
... mounds are here modeled as a channel–levee complex that is characterized by an alternating history of aggradation punctuated by erosional sediment bypass. Levee mudstones have an erosional base, contain dolomitized peloidal thin beds, and have limited faunal constituents. Primary levees were initiated...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2001
AAPG Bulletin (2001) 85 (1): 85-113.
... that has chert nodules, (3) clean dolomite mudstone that has nodular chert, (4) nodular to bedded chert, (5) autoclastic chert, (6) autoclastic chert that has clay infill, and (7) bioclastic wacke-grainstone. The uppermost cycle was terminated by another lithofacies, a chert conglomerate of Mississippian...
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