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Caney Shale

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Journal Article
Published: 01 March 1933
Journal of Paleontology (1933) 7 (1): 3-29.
Journal Article
Journal: AAPG Bulletin
Published: 01 September 2014
AAPG Bulletin (2014) 98 (9): 1739-1759.
... distribution of potential source rocks in the Woodford–Chattanooga and Fayetteville–Caney shale-gas systems. The Woodford–Chattanooga shale is a transgressive deposit that accumulated on an arid continental margin influenced by marine upwelling and minimal sediment influx. A broad HGR depocenter along...
FIGURES | View All (9)
Journal Article
Published: 01 March 1962
Journal of Paleontology (1962) 36 (2): 355-357.
.... choctawensis, originally described from the Caney Shale Upper Mississippian of Oklahoma, becomes a senior synonym. A more finely lirate species of goniatite, found in the Caney Shale, the upper part of the Moorefield Formation of Arkansas, and the lower part of the Chainman Shale of Utah, which occurs some...
Journal Article
Published: 01 September 1945
Journal of Paleontology (1945) 19 (5): 490-503.
Journal Article
Journal: GSA Bulletin
Published: 01 January 1912
GSA Bulletin (1912) 23 (1): 457-462.
...J. B. WOODWORTH Abstract Introduction The Caney shales, described by Taff 2 in 1904, were later characterized as a formation by Girty 3 in the following terms: “The Caney shale occurs in numerous exposures through the Arbuckle and Ouachita Mountains, in the central parts of the Choctaw...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1956
AAPG Bulletin (1956) 40 (2): 428-429.
...Maxim K. Elias ABSTRACT Lithologic monotony and peculiarity of rarely encountered marine faunas are characteristic of the Caney shale facies of Oklahoma. Detailed study of the goniatites and the conodonts (by far the most common among its fossils), provide important paleontologic control...
Series: AAPG Special Publication
Published: 01 January 1956
DOI: 10.1306/SV16348C3
EISBN: 9781629812458
... Abstract The Mississippian Caney shale of the northern Arbuckle Mountains is differentiated into three new members, the Ahlosa, the Delaware Creek, and the Sand Branch, in ascending order. The change of the goniatite faunas from the Sand Branch down to the Delaware Creek is so complete...
Series: AAPG Special Publication
Published: 01 January 1956
DOI: 10.1306/SV16348C23
EISBN: 9781629812458
... Abstract Although Taff originally applied the term “Caney shale” to strata of late Mississippian and early Pennsylvanian age, most writers now restrict the term to Mississippian shale above the Sycamore limestone. Tomlinson applied the term “Springer formation” to that part of Taff’s Caney...
Series: AAPG Special Publication
Published: 01 January 1962
DOI: 10.1306/SV23356C11
EISBN: 9781629812373
... facies exposed only in small slivers in the western part of the Ouachita Mountains in Oklahoma. The former comprise, from oldest to youngest, the Stanley shale, Jackfork sandstone, Johns Valley shale, and Atoka formation. In the frontal zone they comprise, from oldest to youngest, the Caney shale...
Journal Article
Published: 01 November 1960
Journal of Paleontology (1960) 34 (6): 1202-1206.
... of the Barnett formation of Texas, and the Delaware Creek member of the Caney shale is primarily one of geographic province rather than a time disparity. The Illinois basin represents one faunal province, the indicated portions of the Barnett and Caney represent another, and the area of this study shows...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1934
AAPG Bulletin (1934) 18 (8): 971-1009.
... margin of the Oklahoma structural salient and the other is revealed in all portions of the Ouachita region south and east of the Ti Valley-Choctaw belt. The only rocks here assigned a Mississippian age are included in the Caney shale. They measure a few hundred feet in thickness and all their exposures...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1958
AAPG Bulletin (1958) 42 (2): 272-309.
...Charles E. Weaver ABSTRACT X-ray diffraction analysis of Upper Mississippian-Lower Pennsylvanian shales from the Ardmore and Anadarko basins indicates that the Meramecian Caney shales are characterized by the abundance of illite and the scarcity of chlorite and kaolinite, the Chester shales...
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Series: AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C6
EISBN: 9781629812427
... 310 feet of compact, tough, blocky, slate blue, silty to sandy limestone, massive at the base, thick bedded near the middle, and thin bedded toward the top; eastward from the type locality, the upper portion gives way to the lower Caney shale. The massive portion of the Worthey forms the prominent...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1972
AAPG Bulletin (1972) 56 (6): 1087-1099.
... and paleontologically distinct from the lower Springer shale units and the Goddard Formation. The Goddard and Springer Formations are grouped together on the basis of their strong lithologic similarities. The term “Noble Ranch Group” is proposed to include those strata from the top of the Caney Shale to the base...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1959
AAPG Bulletin (1959) 43 (7): 1778-1779.
... part of the area than in the western part. Incompetent shale zones constituted gliding planes along which thrust movement took place, with the principal ones being the Womble shale, Springer formation, Caney shale, Stanley shale, and Johns Valley shale. One can postulate from indirect evidence...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1937
AAPG Bulletin (1937) 21 (1): 1-29.
... the Paleozoic strata are overlapped by beds of the Lower Cretaceous Trinity sand of the Gulf Coastal Plain, which dip gently southward. On the west side of Black Knob Ridge, south of Stringtown, the Caney shale, Springer formation, and Atoka formation of the facies or sequence characteristic of the Arbuckle...
FIGURES
Journal Article
Journal: Geology
Published: 01 July 1988
Geology (1988) 16 (7): 627-630.
... siderophiles occurs in the overlying Caney Shale; the interval contains the following peak concentrations: Ir = 0.56 ppb, Pt =150 ppb, Os = 0.51 ppb, Co = 725 ppm, and Ni =1450 ppm. These elements vary in proportion to the Al (clay) content and we suspect that they were carried in with detrital material from...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1965
AAPG Bulletin (1965) 49 (10): 1666-1679.
... Ouachitas), it becomes thinner, includes more light-colored shale, has fewer and thinner spiculite strata, and the number and thickness of sandstone beds increase. The Wesley shales are interpreted to be equivalent to the upper part of the Caney Shale of the frontal zone. Deposition was on or very near...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1934
AAPG Bulletin (1934) 18 (9): 1132-1159.
... is believed to be largely Burlington in age. Chert in the vicinity of Batesville, Arkansas, which Girty believes to be of Warsaw age, should not be referred to the Osage group. Evidence indicates that the lower Caney shale of the Arbuckle Mountain region is not the clastic equivalent of the Osage group...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1981
AAPG Bulletin (1981) 65 (8): 1501.
... as a sand shadow on the lee side of growing structures. The sands were subsequently winnowed of clay and silt. (c) Truncation of the upper part of the Caney shale on local structures indicates early structural growth. (d) The 3–D seismic survey at East Ardmore supports the idea that the Goddard sands...