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South Mayes field

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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1947
AAPG Bulletin (1947) 31 (3): 495–499.
... that the theories accompanying this presentation of facts are controversial but they are advanced with the thought that broader consideration may lead to clarification. The South Mayes field is located in west-central Chambers County, in the north part of a sector of the coast where widespread faulting...
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Image
<span class="search-highlight">South</span> <span class="search-highlight">Mayes</span> <span class="search-highlight">Field</span> Chambers County, Texas
Published: 01 March 1947
Fig. 1. South Mayes Field Chambers County, Texas
Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/13632144M1163785
EISBN: 9781629812854
... and predictable facies trends. Figure 3. Sub-Mayes unconformity. (A) Location 15, south high-wall section, with small-scale paleotopography expressed as an irregular surface. (B) Location 13, illustrating dip of Pryor Creek Formation across paleotopographic high along the top of the Boone Group, here...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1947
AAPG Bulletin (1947) 31 (6): 1071–1077.
... Mayes field in Chambers County had 2 oil wells, 1 gas well, and 2 dry holes at the close of the year. Production is from the second upper Frio sand. Producing levels and results indicate the field is divided by numerous small faults and separated and controlled by a large strike fault. Only a small area...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1949
AAPG Bulletin (1949) 33 (6): 966–978.
... in the district was completed in the South Mayes field, Chambers County. Production is from the lower Frio at 12,021-12,026 feet. Field development was active on all types of structures. More success was obtained on old piercement salt domes and it was the discovery of these new fault segments and new sands...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1927
AAPG Bulletin (1927) 11 (12): 1307–1320.
... than Boone and may be accounted for by assuming different conditions of sedimentation in north-central Oklahoma in Meramecian and Chesterian times, from the conditions prevailing in south-central Oklahoma and the eastern part of the state. It has been suggested that this cherty part of the Mayes...
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Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/13632142M1163785
EISBN: 9781629812854
... clarification as to which “Moorefield” is beingdiscussed. The proposed type locality for the Pryor Creek Formation is the Pryor Quarry in central Mayes County (location 15) and the unit derives its name from the Pryor Creek tributary of the Grand River south of the town of Pryor ( Figure 3 ). All or most...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1921
AAPG Bulletin (1921) 5 (2): 117–153.
..., but which is correlated by the writers with the Mayes or middle member of the Mississippi lime. The interval between the Salt sand and the Mississippi lime from south to north is as follows: T. 15 N., 800 feet; T. 16 N., 650 feet; T. 17 N., 500 feet; T. 18 N., 450 feet; T. 19 N., 350 feet. The Chattanooga...
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Book Chapter

Author(s)
G. Carl Hale
Series: AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C14
EISBN: 9781629812427
...Abstract Abstract The Southwest Ardmore field is a north-south elongate anticline that plunges to the north and south. It is adjacent to, and on the east flank of, the Criner Hills and separated by a fault on the southwest which defines production. There is more than 1,400 feet of structural...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1968
AAPG Bulletin (1968) 52 (2): 282–294.
...David E. Ogren ABSTRACT Recommendations are made for a revision of terminology and correlations in the Upper Mississippian strata of northern Arkansas. The terms “Mayes Group” and “Hindsville Formation” are applied as they are used in northeast Oklahoma, the term “Ruddell Shale” is recommended...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1936
AAPG Bulletin (1936) 20 (7): 951–974.
... east-west fault and associated cross faults, post-Wapanucka in age. The field is controlled on the west and the south by faults, on the north by dip of over 500 feet to the mile on the subsurface formations, and will probably be controlled on the east by regional dip. 2 Carter Oil Company. ©...
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Series: AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C9
EISBN: 9781629812427
...Abstract Abstract The South Palacine field, located in Sees. 16, 21, 22, 23, 26, 27, 28, and 34, T. 2 S., R. 6 W., Stephens County, Oklahoma, was discovered in May 1049. Principal production comes from several sandstone zones in the Hoxbar sequence of upper Pennsylvanian age. Structurally...
Series: AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C13
EISBN: 9781629812427
...Abstract Abstract The West Brock field, in southern Carter County, Oklahoma, was discovered by H. F. Gibson in February, 1947. To date practically all production has been from Pennsylvanian horizons. Oil is trapped in several closures against the south side of east-west trending normal faults...
Journal Article
Published: 01 November 2003
Vadose Zone Journal (2003) 2 (4): 664–676.
... . Preferential flow through intact soil cores: Effects of matric head . Soil Sci. Soc. Am. J . 63 : 1591 – 1598 . Lindsay , K.A. 1995 . Miocene- to Pliocene-aged suprabasalt sediments of the Hanford site, south-central Washington . BHI-00184 . Bechtel Hanford, Inc ., Richland, WA . Mayes...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1934
AAPG Bulletin (1934) 18 (9): 1132–1159.
... (1930 , p. 559) believes that the upper Burlington beds are missing in Oklahoma. About a mile and a half northwest of Salina, Oklahoma, on the south side of the Pryor road, an Osage inlier rises through the younger Mayes formation. This hill has been cited by several previous writers as one...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1927
AAPG Bulletin (1927) 11 (10): 1097–1108.
... the oil fields as of August, 1927. The limit of the plateau probably falls within the boundary of this map, but cannot be defined more closely at the present time. Width of map, 18 miles. Many dry holes and a few shallow-sand producers had been drilled north of the Arbuckle Mountains and south...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1938
AAPG Bulletin (1938) 22 (11): 1560–1578.
.... These beds of thin calcareous grit are commonly called “False” Mayes in the field. Thin lenticular beds of dark brown limestone are present in the upper part, and a bed of globular glauconite ordinarily identifies the top. As the top is generally difficult to place, it can not be relied on for detailed...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1939
AAPG Bulletin (1939) 23 (3): 325–338.
... of the best exposed sections in the region. The writer wishes to acknowledge the work of Clarence Brehm and Edward Lane, of Tulsa, in assisting in preparation of the sections; and the work of Lewis M. Cline, of Iowa State College, in field assistance. 1 Manuscript received, November 9, 1938. 2...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1949
AAPG Bulletin (1949) 33 (5): 695–719.
... of the major fault of the area where it was locally preserved from pre-Deese erosion. It has been identified as far south as T. 6 N., R. 3 W., and as far north as the South Moore pool in T. 10 N., R. 3 W. However, it is missing in the West Moore field and northwestern Cleveland County. The maximum thickness...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1975
AAPG Bulletin (1975) 59 (4): 633–664.
... in the north, the Moorefield, with the shale of the “Ada-Mayes” (basal Caney) in the south, and then extended this correlation to the sandstones of the Sycamore-Caney on the south side of the Arbuckle Mountains. The Osage was shown to disappear southward by a combination of truncation and onlap...
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