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Boktukola Syncline

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Journal Article
Journal: AAPG Bulletin
Published: 11 November 1996
AAPG Bulletin (1996) 80 (11): 1695-1709.
... in the Lynn Mountain syncline. Similar sequences may also exist well to the south, in the Boktukola syncline, where thick sand intervals have been identified. Petrographic study of samples from the Lynn Mountain syncline suggests that channel sequences may have significantly higher reservoir quality than...
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Series: AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C16
EISBN: 9781629812427
... described by Honess from McCurtain County (Honess, 1924). More than 6,000 feet of Atoka is exposed, but the top of this formation is not in evidence. The trace of the Boktukola fault as seen on the state geologic map was corrected. A new large thrust fault, the Cloudy fault, was mapped and named...
Image
—Regional cross section showing position of current Jackfork gas play relat...
Published: 11 November 1996
Figure 3. —Regional cross section showing position of current Jackfork gas play relative to dominant structure. Note presence of Jackfork strata well to the south, in the Lynn Mountain and Boktukola synclines. The Sohio-Weyerhaeuser 1-22 well, located on the Broken Bow feature, penetrated low
Image
—Composite figure showing (a) locations (designated by large black circles)...
Published: 11 November 1996
Figure 10. —Composite figure showing (a) locations (designated by large black circles) where channel facies have been identified in the Jackfork; (b) a north-south structural cross section through the Lynn Mountain and Boktukola synclines showing surface and subsurface distribution of probable
Image
Figure 3. Simplified geological map of the central Ouachita fold-and-thrust...
Published: 01 May 2006
Figure 3. Simplified geological map of the central Ouachita fold-and-thrust belt and Arkoma Basin with mean joint azimuth of the most-frequent joint set plotted for selected outcrops. Major thrust faults (Boktukola, Octavia, Windingstair, Choctaw) are traced with bold lines. Imbrications
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1971
AAPG Bulletin (1971) 55 (8): 1366-1368.
... method in analysis of sediments : New York, McGraw-Hill , 508 p. Hart , O. D. , 1963 , Geology of the eastern part of Winding Stair Range, LeFlore County, Oklahoma : Oklahoma Geol. Survey Bull . 103 , 87 p. Shelbourne , O. B. , Jr. , 1960 , Geology of the Boktukola syncline...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1936
AAPG Bulletin (1936) 20 (4): 479-491.
... and well established to require further comment. Probably no Ouachita boulder moved many miles from its source. All the known boulders are along the north side of the mountains; none is known in the Boktukola syncline in the interior where the apparently continuous succession represents much more than...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1965
AAPG Bulletin (1965) 49 (10): 1666-1679.
... Jackfork, and there is some doubt regarding which of these is the Markham Mill and which is the Wesley. The southward decrease in highly siliceous shale layers of the Stanley and Jackfork was discussed previously by Shelburne (1960, p. 57). Mapping south of the Octavia fault in the Boktukola syncline...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1967
AAPG Bulletin (1967) 51 (4): 504-528.
..., on the southern flank of the Tuskahoma syncline near Moyers, Oklahoma, the Moyers, is about 1,100 feet thick and consists of a 1–2-foot-thick basal gray siliceous shale overlain by a sequence of gray, green, olive-green, and greenish gray shale with flaky, splintery, or conchoidal structure and irregularly bedded...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1971
AAPG Bulletin (1971) 55 (3): 387-402.
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1963
AAPG Bulletin (1963) 47 (10): 1840-1854.
... of the Boktukola syncline, southeastern Oklahoma : Okla. Geol. Survey Bull. 88 , 84 p. Simons , D. B. , and Richardson , E. V. , 1961 , Forms of bed roughness in alluvial channels : Proc. Amer. Soc. Civil Engineers, Jour. Hydraulics Div., HY 3 , p. 87 – 105 . Sullwold , H. H. , 1960...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1958
AAPG Bulletin (1958) 42 (11): 2757-2765.
... is concealed beneath alluvium and terrace gravels of the Poteau River throughout much of its extent in the Waldron Quadrangle, Reinemund and Danilchik point out that “It truncates obliquely the north-dipping rocks in the south limb of the Poteau syncline and the north-dipping rocks of the Choctaw anticline...
Journal Article
Journal: GSA Bulletin
Published: 01 May 2006
GSA Bulletin (2006) 118 (5-6): 710-723.
...Figure 3. Simplified geological map of the central Ouachita fold-and-thrust belt and Arkoma Basin with mean joint azimuth of the most-frequent joint set plotted for selected outcrops. Major thrust faults (Boktukola, Octavia, Windingstair, Choctaw) are traced with bold lines. Imbrications...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1966
AAPG Bulletin (1966) 50 (2): 308-326.
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1958
AAPG Bulletin (1958) 42 (11): 2765-2783.
... reference to Honess’ actual use of the terms “thrust,” “thrust folding,” and “thrust faulting,” is somewhat less than conducive to conveying an objective picture. It should be added that the Boktukola fault at the northern border of the belt under discussion is represented in Honess’ cross sections...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1975
AAPG Bulletin (1975) 59 (6): 974-985.
... on the north by the Windingstair fault and on the south by the Broken Bow uplift. It contains three large synclines in the Carboniferous flysch sequence and fewer reverse faults than the frontal Ouachita province. The southeasternmost province, the Broken Bow uplift, consists of Ordovician through Devonian...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1931
AAPG Bulletin (1931) 15 (9): 991-1057.
...) have published the most recent studies of these mountains. The chain is expressed in three en échelon west-northwest and east-southeast striking ridges of granite, with injections of gabbro and porphyry. A deep syncline, now compressed into a very narrow trough, 8,000 feet deep, separates...
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