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Ardmore

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Series: Geological Society, London, Memoirs
Published: 30 October 2020
DOI: 10.1144/M52-2017-34
EISBN: 9781786205070
... Abstract The Alma Field (formerly Argyll and then Ardmore) is located within Blocks 30/24 and 30/25 on the western margin of the Central Graben. Hamilton drilled the first discovery well 30/24-1 in 1969 and the field, named ‘Argyll’, became the first UK offshore oilfield when production...
FIGURES | View All (10)
Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2005
DOI: 10.1144/0060367
EISBN: 9781862394124
... and the facilities removed. In January 2002 two new oil companies, Tuscan Energy and Acorn Oil and Gas, were awarded the licence to redevelop the Argyll Field - now renamed Ardmore. A field development plan was submitted to the DTI and approval granted in October 2002. The first Ardmore well was drilled...
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Journal Article
Published: 01 October 2003
Petroleum Geoscience (2003) 9 (4): 295–307.
... Formation as a whole forms a high quality reservoir at depths of 3000–4000 m. The best intervals, with Darcy permeabilities, consist of coarse-grained Weissliegend sands. Two of the four initial wells in the Ardmore (Argyll) Field redevelopment are planned to target the Rotliegend reservoir. 11 8 2003...
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Journal Article
Published: 01 March 1994
Journal of Paleontology (1994) 68 (2): 223–233.
Series: DNAG, Centennial Field Guides
Published: 01 January 1988
DOI: 10.1130/0-8137-5404-6.189
EISBN: 9780813754109
... Abstract The two lower members of the Springer Formation are well exposed in the vicinity of City Lake, located northwest of Ardmore, Oklahoma. The upper member of the Springer Formation and the lower member of the Golf Course Formation are well exposed along Phillips Creek, northwest...
... Abstract A seismic profile from the Ardmore basin illustrates a positive flower structure and demonstrates important criteria for identifying convergent (or transpressional) wrench faults with seismic control. Positive flower structures are linear antiforms that are cut longitudinally along...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1981
AAPG Bulletin (1981) 65 (8): 1501.
...J. S. Vietti; S. D. Adams Abstract Chevron and three partners began developing the East Ardmore structure near Ardmore, Oklahoma, in 1974–75. The discovery well and first offset both produced gas from the Mississippian Goddard sands. The drilling program was abruptly halted when a zero sand well...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1979
AAPG Bulletin (1979) 63 (1): 106–109.
...Virgil H. Roan 1 Manuscript received, May 17, 1978; accepted, June 23, 1978. 2 Geologist, Ardmore, Oklahoma 73401. © 1979 American Association of Petroleum Geologists. All rights reserved. 1979 American Association of Petroleum Geologists The science of geology...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1972
AAPG Bulletin (1972) 56 (6): 1087–1099.
...) in age. The systemic boundary is placed at, or near, the base of the Lake Ardmore Member of the Springer Formation. Pre-Lake Ardmore strata are characterized by the Chesteran conodont species Adetognathus unicornis and Gnathodus girtyi intermedius . Early Morrowan conodonts, including Spathognathodus...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1966
AAPG Bulletin (1966) 50 (7): 1365–1374.
...-scale low-angle thrusting, although seismic data indicate moderately dipping thrust or reverse faults. The eastern part of the Ardmore basin is dominated by three major faults, the Cumberland, Aylesworth, and Southeast Madill. Four prolific oil fields are located in the basin area. The Meers Valley...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1966
AAPG Bulletin (1966) 50 (7): 1518.
... by Bruce Harlton on the “Relation of buried Tishomingo uplift to Ardmore basin and Ouachita Mountains, southeastern Oklahoma” (p. 1365, this issue) is of great interest to me because of the extensive lease play (now unfortunately defunct) which was initiated by J. V. Howell and me about 1950. This area has...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1966
AAPG Bulletin (1966) 50 (7): 1519.
... mainly of green to emerald-green, siliceous shale and novaculite. Both lithologic units also are present in the equivalent Woodford in the Ardmore basin. The Arkansas Novaculite is underlain by the Polk Creek Shale (8,400-8,432 feet). The upper 20 feet consists of light green shale and the lower 12 feet...
Journal Article
Journal: GSA Bulletin
Published: 01 June 1963
GSA Bulletin (1963) 74 (6): P95–P96.
Series: AAPG Special Publication, AAPG Special Publication
Published: 01 January 1962
DOI: 10.1306/SV23356C13
EISBN: 9781629812373
... Abstract During Pennsylvanian time, the Ardmore basin was the site of almost continuous deposition in long, narrow, and oftendeep basins lying in close proximity to structurally and topographically high islands. These islands and sea-mount archipelagoes formed and were rejuvenated during...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1961
AAPG Bulletin (1961) 45 (4): 556–560.
... sandstones 3 exposed in the Ardmore basin and of cores taken from similar formations in the subsurface of the Anadarko basin. It was hoped such a study would reveal discriminating heavy-mineral assemblages that would provide a sound basis for positive identification of subsurface sands from field to field...
FIGURES
Series: AAPG Special Publication, AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C1
EISBN: 9781629812427
... Abstract During Pennsylvanian time, the Ardmore basin was the site of almost continuous deposition in long, narrow, and often deep basins lying in close proximity to structurally and topographically high islands. These islands and sea-mount archipelagoes formed and were rejuvenated during...
Book Chapter

Author(s)
G. Carl Hale
Series: AAPG Special Publication, AAPG Special Publication
Published: 01 January 1959
DOI: 10.1306/SV19352C14
EISBN: 9781629812427
... 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 relief...