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Ouachita-Arbuckle sediments

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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1937
AAPG Bulletin (1937) 21 (1): 1–29.
..., that in Bigfork time the Ouachita and Arbuckle basins of sedimentation were connected and that there was a gradual change westward from more siliceous deposits to more calcareous deposits. It is the writers’ opinion that northwestward thrusting along the Choctaw fault has moved the rocks of Black Knob Ridge...
FIGURES
Series: AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C1
EISBN: 9781629812427
... were first formed during this period of unrest. Concomitant erosion of these islands stripped as much as 8,000-13,000 feet of sediments from many of them before their burial in late Desmoinesian time. The Atokan Series began with the deposition of thick conglomerates in the vicinity of the Criner...
Series: AAPG Special Publication
Published: 01 January 1962
DOI: 10.1306/SV23356C11
EISBN: 9781629812373
... of extreme southwestern Texas, and crosses the border into Mexico. In the outcrop areas, and throughout the length of the Ouachita structural belt, these rocks show strong similarities in lithologic character, fabric, and meta-morphic grade, which may be used to differentiate them from sediments of foreland...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1956
AAPG Bulletin (1956) 40 (2): 423–424.
...J. Kaspar Arbenz ABSTRACT Oklahoma can be divided into the following major tectonic units: The Oklahoma salient of the Ouachita Mountain orogen with the McAlester-Arkansas basin as foredeep. The Arbuckle Mountain-Criner Hills-Wichita orogenic system with the Anadarko basin as foredeep. The cratonic...
Series: AAPG Special Publication
Published: 01 January 1962
DOI: 10.1306/SV23356C13
EISBN: 9781629812373
... amounts of oil were first formed duringthis period of unrest. Concomitant erosion of these islands stripped as much as 8,000-13,000 feet of sediments from many of them before their burial in late Desmoinesian time. The Atokan Series began with the deposition of thick conglomerates in the vicinity...
Journal Article
Journal: GSA Bulletin
Published: 01 April 1953
GSA Bulletin (1953) 64 (4): 421–442.
... Ouachita Mountains and the Arbuckle Mountains and McAlester Basin. The former group consists largely of chert and siliceous shale of typical geosynclinal facies; the latter group consists largely of chert and siliceous limestone intermediate in lithology and fabric between rocks of geosynclinal facies...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1941
AAPG Bulletin (1941) 25 (9): 1619–1705.
..., Missouri; and Sioux Falls district, South Dakota. Great thicknesses of Upper Cambrian and Ordovician rocks, dominantly limestones, are exposed in the Llano uplift and the Arbuckle and Wichita mountains. The Ouachita Mountains, Oklahoma and Arkansas, present a sequence of Cambrian and Ordovician rocks...
FIGURES | View All (16)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1931
AAPG Bulletin (1931) 15 (9): 991–1057.
... - 20,000 feet of Stanley-Jackfork (Mississippian-Pennsylvanian) sediments. not represented in the Arbuckle Mountains. The clastic Stanley-Jackfork sediments of the Ouachita Mountains are comparable, in their broader structural relations, with the fiysch fades of Europe. 1 They must be considered...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1958
AAPG Bulletin (1958) 42 (1): 212.
...B. W. Miller ABSTRACT The McAlester-Arkansas Coal basin is an elongate arcuate basin in southeastern Oklahoma and northwestern Arkansas. It is bounded by the following: Mississippi embayment on the east, Ozark uplift on the north, Ouachita Mountains on the south, and Arbuckle Mountains on the west...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1956
AAPG Bulletin (1956) 40 (2): 425–426.
... was rising, the basin area continued to sink and to receive sediments, partly derived from the eroding Hunton anticline. Local uplift on the northeast flank of the present Arbuckle anticline and north flank of the Tishomingo anticline resulted in pre-Desse erosion of all or parts of the Atoka, Wapanucka...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1981
AAPG Bulletin (1981) 65 (8): 1496–1497.
...., Arbuckle province). Silty black shale is more common in the north whereas silicified black shale increases to the south. Overall low rates of clastic sedimentation and high planktonic organic productivity prevailed over the entire region. The small amounts of clastic silt and clay came from the north...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1950
AAPG Bulletin (1950) 34 (3): 618–619.
..., Wichita, Arbuckle, and Ouachita uplifts (increasing in deformation from west to east) and the adjoining Anadarko, Ardmore, and McAlester basins on their flanks; (4) rejuvenated faulting, warping, and over-thrusting, culminating in late Pennsylvanian and early Permian time, that re-elevated these features...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1960
AAPG Bulletin (1960) 44 (1): 126–127.
...William M. Caplan ABSTRACT The Arkansas Valley is an east-west trending synclinorium bounded on the north by the Ozark uplift and on the south by the Ouachita Mountain anticlinorium. The Valley is an eastward extension of the McAlester basin of southeastern Oklahoma. Pennsylvanian Atoka sediments...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1952
AAPG Bulletin (1952) 36 (8): 1671–1672.
...John G. Bartram A large proportion of the Pennsylvanian sediments in the Mid-Continent area are dark shales, which tend to grade eastward into sandstones, and westward into limestones. Most of this dark shale is believed to have come from a land mass (Llanoria), located to the southeast. The large...
Image
—A. Generalized geologic map of south-central United States showing approxi...
Published: 01 June 1983
FIG. 1. —A. Generalized geologic map of south-central United States showing approximate location of COCORP traverses across Ouachita Mountains in western Arkansas. Brick pattern = lower to middle Paleozoic platform sediments (“Arbuckle facies”); solid black = lower to middle Paleozoic deep-water
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1953
AAPG Bulletin (1953) 37 (4): 778–796.
...Bruce H. Harlton ABSTRACT The writer proposes an alternative explanation of the sharply contrasted lithologic character of the Paleozoic sediments (Ordovician to Lower Mississippian) in the Arbuckle Mountains and the Ouachita Mountains, respectively. Although only 12 miles separate the two facies...
FIGURES | View All (9)
Journal Article
Published: 01 January 1991
Journal of Sedimentary Research (1991) 61 (1): 28–42.
...) exposed in the western portion of the Mill Creek Graben, Arbuckle Mountains, Oklahoma. The sequence was deposited in shallow marine shelf setting within a tectonically active basin; deposition was strongly influenced by adjacent terrigenous coastal depositional environments. The section was synclinally...
Series: SEPM Special Publication
Published: 01 January 1981
DOI: 10.2110/pec.81.31.0071
EISBN: 9781565761612
... Abstract The Antlers Formation is a Cretaceous fluvial, deltaic, and strandplain unit up to 300 m thick that accumulated basinward of the Wichita-Arbuckle-Ouachita highlands, it extends downdip to an arbitrary, nomenclatural southern limit at the landward pinchout of the Glen Rose Formation...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1936
AAPG Bulletin (1936) 20 (10): 1342–1356.
... and Savanna sandstones. Much of the deposition was marine in the western part and continental or very shallow water in the eastern part of the coal basin. The source of the sediments is believed to be (1) Llanoria, (2) the previously deposited Stanley, Jackfork, and Atoka of the Ouachita Mountains, (3...
FIGURES | View All (5)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1964
AAPG Bulletin (1964) 48 (4): 551.
... and deep subsidence of adjacent grabens delineated by this major fault system, have exerted a profound control over the stratigraphic and structural evolution of southern Oklahoma. The larger faults, the Meers fault of the Wichita Mountains, the Washita Valley and Sulphur faults of the Arbuckle Mountains...