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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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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
Journal: AAPG Bulletin
Published: 01 March 1975
AAPG Bulletin (1975) 59 (3): 486–509.
... consists basically of an ascending sequence of: thick, locally nonmarine (“outside”) shale–thin middle limestone member–thin black shale member–thick upper limestone member–outside shale. Conodont distribution (chiefly multielement) ranges from (1) low abundance and diversity, commonly with Adetognathus...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1957
AAPG Bulletin (1957) 41 (3): 441–465.
... sandstones that commonly weather to form badlands. The Owl Rock member is composed 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...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1977
AAPG Bulletin (1977) 61 (7): 1045–1068.
... The middle and upper limestone members are separated by the most distinctive of the shale members, the one that commonly contains a black fissile facies, which typically carries nonskeletal phosphorite and lacks benthic fossils. Although sometimes absent in this shale member, the phosphatic black facies...
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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
Journal: AAPG Bulletin
Published: 01 May 1969
AAPG Bulletin (1969) 53 (5): 1058–1074.
... the mound into upper and lower massive units. Captain Creek Limestone Member (Stanton Formation) in Table Mound quarry near Independence, Montgomery County, Kansas. FIG. 5. —Massive vuggy limestone of algal mound abruptly overlying thin-, well-bedded limestone typical of open marine facies...
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Image
FIGURE 1 —A) Study localities in Sarpy and Cass counties, Nebraska (see  Ap...
in > PALAIOS
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
Journal Article
Published: 01 May 2005
Journal of Sedimentary Research (2005) 75 (3): 350–368.
... in the TST and HST, in later sections. 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...
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Journal Article
Journal: PALAIOS
Published: 01 September 2014
PALAIOS (2014) 29 (9): 483–494.
.... To address the validity of these dietary and habitat inferences, patterns of dental microwear obtained from low-magnification stereomicroscopy for C. williamsi specimens from Sterkfontein Member 4 (n = 13) are compared to a broad comparative sample of extant primates, including Cebus apella (n = 10), Colobus...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2007
GSA Bulletin (2007) 119 (3-4): 391–412.
... and the Paleocene to Eocene transition. The Paleocene through lowermost Eocene succession is >100 m thick and was deposited at middle to lower bathyal depths in a hemipelagic, near-continental setting in the central western Tethys. In the Forada section, the Paleocene succession of limestone-marl couplets...
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Image
—Photographs of the basal boundary of the Tonganoxie sequence. (a) Outcrop ...
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 (...
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 September 1969
AAPG Bulletin (1969) 53 (9): 1866–1879.
... of Early and Middle(?) Triassic age; in ber of the Dolores Formation ( Fig. 1 ). The redbed sequence consists of reddish-brown, horizontally bedded or structureless siltstone and minor amounts of limestone and sandstone. It includes members in the upper part of the Chinle Formation, a lower member (Rock...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 2014
AAPG Bulletin (2014) 98 (9): 1789–1809.
... modeling. In this outcrop–based study, we generated a data set of the dimensions of fracture–related dolomite geobodies hosted in Ediacaran (Khufai Formation) limestones of the Oman Mountains that are up to several hundreds of meters long and a few tens of meters wide. The dolomite formed under burial...
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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
Published: 01 January 2000
Journal of Paleontology (2000) 74 (1): 72–083.
... taxa described here but no diagnostic plates are seen. These specimens are best left unassigned at this time. These three specimens were collected from an abandoned quarry near Garnett, Kansas (Locality 2) from surface float of the Stoner Limestone Member of the Stanton Formation (Missourian...
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Journal Article
Published: 01 May 2007
Journal of the Geological Society (2007) 164 (3): 685–688.
... of the Bembridge Limestone, the base of sequence 5 of Gale et al . (2006) (their intervening sequences 6 and 7 within the Bembridge Marls and lower Hamstead members being poorly defined). Subchron I in Chron C13r therefore provides the best fit for the Bembridge normal polarity zone. The stratigraphical...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 April 2001
GSA Bulletin (2001) 113 (4): 469–481.
... South, and Cava Termini sections (Lima Valley, northern Tuscany). In Lima Valley, the Tuscan Cherts overlie turbiditic cherty limestones of the Calcare Selcifero della Val di Lima and are overlain by the Maiolica Formation. The lower Chert sensu stricto member at Monte Pratofiorito is divided into 4...
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