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Stoner Limestone Member

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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1984
AAPG Bulletin (1984) 68 (2): 150–163.
.... During regressive depositional phases in the Missourian (Late Pennsylvanian), siliciclastic sediments were transported into Kansas mainly from the southeast. The five members of the latest Missourian Stanton Formation (in ascending order: Captain Creek Limestone, Eudora Shale, Stoner Limestone, Rock Lake...
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Journal Article
Journal: PALAIOS
Published: 01 December 2008
PALAIOS (2008) 23 (12): 833–847.
...R. M. Joeckel Abstract Enigmatic structures in the shape of inverted rounded cones are very common in a discrete horizon of the upper Stoner Limestone Member (Stanton Limestone Formation, Lansing Group, Upper Pennsylvanian) in southeastern Nebraska. These structures are 100–300 mm in diameter...
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FIGURE 1—A) Study localities in Sarpy and Cass counties, Nebraska (see Appendix 1). B) Stoner Limestone Member at locality 1, with underlying Eudora Shale Member (EuS) containing black phosphatic shale, and overlying Rock Lake Shale, reddish-brown mudstone containing well-developed paleosol (Joeckel, 1989). Sea-level curve is based on Heckel et al. (1979). See text for description of intervals I–VI
Published: 01 December 2008
FIGURE 1 —A) Study localities in Sarpy and Cass counties, Nebraska (see Appendix 1 ). B) Stoner Limestone Member at locality 1, with underlying Eudora Shale Member (EuS) containing black phosphatic shale, and overlying Rock Lake Shale, reddish-brown mudstone containing well-developed paleosol
Image
—Photographs of the basal boundary of the Tonganoxie sequence. (a) Outcrop in an interfluvial area. Basal sequence boundary is at the base of the exposed section, and the grassy slope covers the Iatan Limestone. The lower arrow points to a coal, possibly the Upper Sibley Coal, and the upper arrow points to the Haskell Limestone, which is generally thin in interfluvial areas. Units on the scale are 15 cm. (b) Basal sequence boundary near the middle of the trunk paleovalley. The top of the hammer rests on the boundary between the Stoner Limestone Member of the Stanton Limestone below and conglomeratic facies of the Tonganoxie Sandstone Member of the Stranger Formation above. The hammer is 28 cm. (c) Outcrop at the Buildex quarry at the edge of the trunk paleovalley. The arrow (left side of the photograph) points to the basal sequence boundary. The Ottawa Coal above the boundary is rooted in the Weston Shale below the boundary. Note the slight discordance between the Weston Shale and the Ottawa Coal.
Published: 01 July 1995
, and the upper arrow points to the Haskell Limestone, which is generally thin in interfluvial areas. Units on the scale are 15 cm. (b) Basal sequence boundary near the middle of the trunk paleovalley. The top of the hammer rests on the boundary between the Stoner Limestone Member of the Stanton Limestone below
Image
Rock Lake Shale paleosol (SB 2) at Ash Grove Quarry, Louisville, Nebraska (location A in Fig. 4). Aridisol-like paleosol with comparatively shallow carbonate nodule horizon (Bk) overlies weathered Stoner Limestone Member, upper 25–40 cm of which has pervasive microkarst under a subaerial exposure surface. Upper part of paleosol profile is greenish gray (g) in color from gleying (Fe3+ reduction) associated with marine transgression, but lower part remains reddish brown to dark reddish brown (rb). Soil horizons (A, Bk, Btk, BCk, Ck) include horizons enriched in carbonate (Bk, BCk, Ck), and both carbonate and illuvial clay (Btk). Marine flooding surface atop paleosol is associated with slight erosion and is overlain by very thin, marine-transgressive shale. Modified from Joeckel (1989).
Published: 01 May 2005
Figure 7 Rock Lake Shale paleosol (SB 2) at Ash Grove Quarry, Louisville, Nebraska (location A in Fig. 4 ). Aridisol-like paleosol with comparatively shallow carbonate nodule horizon (Bk) overlies weathered Stoner Limestone Member, upper 25–40 cm of which has pervasive microkarst under
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1969
AAPG Bulletin (1969) 53 (5): 1058–1074.
... of skeletal calcilutite. The overlying Eudora Shale Member averages 6 ft in thickness in northern Kansas, pinches out locally over the mound complex, and thickens abruptly to 70 ft south of the mound. The Stoner Limestone Member contains two algal-mound complexes. In central Anderson County the member...
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Journal Article
Published: 01 May 2005
Journal of Sedimentary Research (2005) 75 (3): 350–368.
...Figure 7 Rock Lake Shale paleosol (SB 2) at Ash Grove Quarry, Louisville, Nebraska (location A in Fig. 4 ). Aridisol-like paleosol with comparatively shallow carbonate nodule horizon (Bk) overlies weathered Stoner Limestone Member, upper 25–40 cm of which has pervasive microkarst under...
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Journal Article
Published: 01 January 2000
Journal of Paleontology (2000) 74 (1): 72–083.
... float of the Stoner Limestone Member of the Stanton Formation (Missourian, Upper Pennsylvanian). Figure 1 —Phylogenetic relationships among species of Postibulla and Parapostibulla. 1, Strict consensus of the three equally most parsimonious trees. ACTRAN character optimization at numbered...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1995
AAPG Bulletin (1995) 79 (7): 1019–1042.
..., and the upper arrow points to the Haskell Limestone, which is generally thin in interfluvial areas. Units on the scale are 15 cm. (b) Basal sequence boundary near the middle of the trunk paleovalley. The top of the hammer rests on the boundary between the Stoner Limestone Member of the Stanton Limestone below...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1941
AAPG Bulletin (1941) 25 (9): 1745–1767.
... cross-bedded, yellowish to red sandstone. Unit 2 is discontinuous bituminous, thin-bedded limestone, in places associated with gypsum, attaining a thickness of 15 feet, and named the Pony Express limestone member of the Morrison formation. Unit 3 is sandstone or sandy beds about 20 feet thick here named...
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Journal Article
Published: 01 May 2007
Journal of the Geological Society (2007) 164 (3): 685–688.
... ( Hooker et al . 2004 ), which calibrates well with the biostratigraphy. The 2‰ positive shift in freshwater δ 18 O values, recorded in rodent tooth enamel by Grimes et al . (2005) between the Osborne Member and the Bembridge Limestone, has been misinterpreted by Gale et al . (2006 , p. 413...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 April 2001
GSA Bulletin (2001) 113 (4): 469–481.
... marlstone (Siliceous Marlstone member; Fig. 4 ). At the boundary between the Jurassic and Cretaceous, a major paleoceanographic change occurred and siliceous sedimentation was replaced by carbonate-rich pelagic sedimentation dominated by calcareous phytoplankton. These pelagic limestones, ubiquitous...
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Journal Article
Published: 01 November 2007
Environmental & Engineering Geoscience (2007) 13 (4): 355–367.
... (mainly till), 16 m of shale and siltstone, a 27-m–thick sandstone aquifer, and about 174 m of low-permeability shales, siltstones, clays, thin coals and limestones, and thin sandstones. The aquifer, the Mount Carmel Sandstone, is moderately permeable (around 10 −6 m/s) and consists of two sandstone...
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Journal Article
Published: 01 May 2008
Quarterly Journal of Engineering Geology and Hydrogeology (2008) 41 (2): 201–216.
... the Thames and through the lock at Limehouse Reach into the Regent's canal. He is passionate about steam, regularly visiting the Great Dorset Steam Fair, and is a life member of the Swanage steam railway in Dorset and the mid-Hants steam railway (Watercress Line) in Hampshire. Peter Fookes is pre...
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Journal Article
Journal: Geosphere
Published: 06 July 2018
Geosphere (2018) 14 (4): 1935–1960.
... approaches that use machine learning to classify sedimentary facies from multivariate data sets. Most attempts have focused on classifying bulk sedimentary facies (e.g., mudstone, sandstone, marl, and limestone) and have had varying success when models are validated against observed lithofacies ( Dubois et...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1969
AAPG Bulletin (1969) 53 (9): 1866–1879.
... of limestone and sandstone. It includes members in the upper part of the Chinle Formation, a lower member (Rock Point Member) of the Wingate Sandstone, and the upper two members of the Dolores Formation or, locally, the entire Dolores Formation ( Fig. 1 ). The sandstone sequence is composed of light-brown...
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Journal Article
Published: 01 December 2013
Journal of Sedimentary Research (2013) 83 (12): 1114–1129.
... was performed using stratigraphic data from the Pennsylvanian succession containing floodplain limestones of the Stewart Quadrangle of Athens County in Ohio (USA). Limestone volumes for six limestone units (Upper Pittsburgh, Fishpot, Sewickley, Benwood/Arnoldsburg, Uniontown, and Waynesburg limestones) were...
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Journal Article
Published: 22 January 2013
Canadian Journal of Earth Sciences (2013) 50 (5): 564–575.
... pentes de pergélisol ont accru les taux de sédimentation dans le bassin. [Traduit par la Rédaction] Middle Ordovician Bay Fiord Formation bedrock, regionally composed of dolomite and gypsum with limestone, shale, and siltstone underlie the lake. To the southwest and west of the lake...
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Journal Article
Published: 01 February 2001
Geochemistry: Exploration, Environment, Analysis (2001) 1 (1): 61–70.
..., siltstones, limestones, coals and sandstones. A generalized stratigraphic column for the lower part of the Monongahela group is shown in Figure 2. Over much of the basin, limestones and calcareous shales overlie the coal, but rapid facies changes produced channel sandstone roofrock in some areas ( McCullogh...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1957
AAPG Bulletin (1957) 41 (3): 441–465.
... of pale red, dominantly non-bentonitic siltstone and light greenish gray and pale red limestone. The Church Rock member is noticeable as a reddish or brownish siltstone and sandstone unit lying above the limestones of the Owl Rock member. The Chinle formation is a brightly colored slope-forming unit...
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