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Grayburg-Queen sequence

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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 1989
DOI: 10.2110/pec.89.44.0289
EISBN: 9781565761056
...) Cherry Canyon Sandstone Tongue and the overlying shallow-water-to-peritidal dolomite facies of the uppermost Grayburg and overlying Queen Formations. The lowermost one-fourth of Grayburg strata is foreslope facies exhibiting basinward-prograding strata with dips of 5° to 35°. The foreslope strata...
Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2014
DOI: 10.2110/sepmsp.105.13
EISBN: 9781565763241
.... A180-m-relief collapse scar at the margin as exposed at Bush Mountain on the Western Escarpment removed critical evidence of potential reef-margin development for the middle Grayburg-lower Queen sequences. Following this major collapse, the upper Queen (shelf)-Goat Seep (reef)-South Wells (basin...
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Series: SEPM Core Workshop Notes, SEPM Core Workshop Notes
Published: 01 January 1984
DOI: 10.2110/cor.84.05.0136
EISBN: 9781565762602
... that prior to deposition of the Grayburg Formation a regression exposed the underlying carbonate platform. During subsequent transgression, open shelf deposits of the Grayburg formed and were overlain by shallow shelf deposits. The capping regressive sequence comprises shallow shelf-to-intertidal sediments...
Series: SEPM Core Workshop Notes, SEPM Core Workshop Notes
Published: 01 January 1991
DOI: 10.2110/cor.91.01.0429
EISBN: 9781565762695
... Abstract Early Guadalupian Grayburg dolostones and siltstones accumulated on shallow-water to exposed platforms that encircled the Midland Basin, West Texas. The Grayburg Formation is the uppermost of several upward-shoaling sequences of the lower Guadalupian and is transitional between...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1959
AAPG Bulletin (1959) 43 (9): 2197–2213.
... limestone is overlain by the Grayburg formation which is equivalent to the Grayburg formation of subsurface usage. The Grayburg formation and overlying Queen formation are laterally equivalent to the Goat Seep limestone and thus of middle Guadalupe age. 1 Manuscript received, September 12, 1958...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1962
AAPG Bulletin (1962) 46 (4): 504–517.
... “Grayburg” was defined by Dickey (1940 , p. 44–47) as a subsurface sequence of dolomite, anhydrite, and sandstone 299 feet thick in sec. 7 of T. 17 S., R. 30 E., Eddy County, New Mexico. The Grayburg is overlain by the Queen Formation and underlain by the San Andres Formation. Moran (1954) proposed...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1984
AAPG Bulletin (1984) 68 (1): 116–117.
... produced from the Queen and Seven Rivers sandstones, and the Grayburg, San Andres, and Wolfcamp dolomites. All of these zones are productive from stratigraphic traps. The lower Morrow sandstones occur at a depth of about 11,400 ft (3,474 m). They are interpreted to be a prograding fluvial-deltaic sequence...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1946
AAPG Bulletin (1946) 30 (11): 1857–1874.
... genus was known elsewhere only in beds of Leonard age. With the foregoing as a basis, the following pattern was developed. The Whitehorse group, with the exception of the Grayburg formation and part of the Queen formation, was correlated with the Carlsbad and Capitan formations of the Guadalupe...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1963
AAPG Bulletin (1963) 47 (11): 1952–1962.
... and shale that contains veins of satin spar. As Marlow of Oklahoma and Grayburg in Coke County have about the same lithologic character, thickness, and position in the Permian sequence, they are probably the same formation. Tait et al . (1962) traced the Tansill, Yates Seven Rivers, Queen...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1943
AAPG Bulletin (1943) 27 (6): 747–770.
... which is a discovery success of 17.1 per cent. These six producers accounted for three new areas of production and three extensions of known areas. The wildcat discoveries and extensions were all from known Permian producing zones being from the Yates, Queen, Grayburg, and San Andres formations...
FIGURES
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2004
DOI: 10.1306/M81928
EISBN: 9781629810058
... composite-sequence boundaries (green lines), cored-well locations (yellow vertical lines with black boxes that represent core), stratal geometries, and main stratigraphic horizons: Y = Yates; Q = Queen; G = Grayburg; USA = Upper San Andres; LSA = Lower San Andres. Profile B is the same seismic profile...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 2013
AAPG Bulletin (2013) 97 (2): 223–250.
... setting of the early to middle Permian that are available in few other places. They also afford an excellent basis for examining how styles of facies and sequence development vary between inner and outer platform settings. We collected detailed data on the facies composition and architecture of lower...
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Journal Article
Published: 01 September 2010
Journal of Sedimentary Research (2010) 80 (9): 808–828.
.... This locality, in Carlsbad Caverns National Park ( Fig. 1 ), has the most complete Tansill section exposed in the Guadalupe Mountains—illustrating a classical shelf-to-margin profile. In spite of this, little has been published on its sequence-stratigraphic architecture when compared with other formations...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1996
AAPG Bulletin (1996) 80 (4): 460–484.
... billion bbl of oil, from four Guadalupian-age formations: Seven Rivers, Queen, Grayburg, and San Andres. In early 1995, daily production was approximately 55,000 BOPD ( Tinker and Mruk, 1995 ). Fifteen-hundred wells have been drilled on 10-ac spacing through the upper part of the San Andres Formation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1994
AAPG Bulletin (1994) 78 (2): 181–216.
... basin in west Texas and New Mexico during the Permian (Leonardian-Guadalupian) ( Figures 1 , 2 ) ( Ward et al., 1986 ). Reservoirs in the San Andres, and in the Leonardian Clear Fork Group and the middle-late Guadalupian Grayburg, Queen, Seven Rivers, and Yates formations, define a larger genetic...
FIGURES | View All (33)
Journal Article
Published: 01 January 2007
Journal of Sedimentary Research (2007) 77 (1): 34–58.
... ). Boyd (1958) mapped the Grayburg and Queen formations as an undifferentiated succession. Hayes (1964) placed the top of the Grayburg below a "locally conspicuous sandstone" assigned to the Queen Formation. Sarg and Lehmann (1986) interpreted the top of the Grayburg to represent a sequence boundary...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.265.01.02
EISBN: 9781862395138
.... Early Triassic magnetostratigraphic sequences agree quite well ( Fig. 1 ) and display no polarity-biostratigraphy conflicts. This agreement, in such marked contrast to the Mid- and Late Permian or the Late Triassic, is probably due to relatively accurate recording of the geomagnetic field polarity...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1976
AAPG Bulletin (1976) 60 (6): 907–925.
... evaporites and red beds generally are considered to be part of the overlying Grayburg Formation. Because this overall sequence, which extends from siliceous limestone and sandstone at the base upward into evaporites, represents a single progradational unit, it seems likely that the formational “top...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2004
DOI: 10.1306/M80924C2
EISBN: 9781629810478
... ( Borer and Harris, 1989 , 1991a , b ; Mutti and Simo, 1993 ), and others exist in the same basin (e.g. the Queen and Grayburg Formations). In the Yates Formation example of Borer and Harris (1991b) , a series of cores along a dip-oriented transect documents the lateral mixing of silici-clastics...
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Journal Article
Journal: AAPG Bulletin
Published: 15 August 2019
AAPG Bulletin (2019) 103 (8): 1839–1887.
... terminations and internal reflection configurations from this 35-Hz peak-frequency seismic data. The uncertainties in interpreting the G9 top because seismic reflections may follow low-impedance reservoir compartments and thus cross the upper San Andres–Grayburg sequence boundary. These reservoir...
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