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Journal Article

Geology of University Waddell Devonian Field, Crane County, Texas: ABSTRACT Free

David Brimberry
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 553.
DOI: https://doi.org/10.1306/03B59C2E-16D1-11D7-8645000102C1865D
...David Brimberry The primary production in the University Waddell field in Crane County, Texas, is obtained from Devonian siliceous carbonates. Since its discovery in 1948, the field has produced 42 million bbl of oil through primary and secondary production. The field’s structure is an asymmetric...
View PDF for article title, Geology of <span class="search-highlight">University</span> <span class="search-highlight">Waddell</span> Devonian <span class="search-highlight">Field</span>, Crane County, Texas: ABSTRACT
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Structural geologic map of Thirtyone Formation, University Waddell field, Crane County, Texas.

Structural geologic map of Thirtyone Formation, University Waddell field, C... Available to Purchase

Published: 31 August 2006
Figure 2. Structural geologic map of Thirtyone Formation, University Waddell field, Crane County, Texas.
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Logs of type well University Waddell field, Crane County, Texas. Location of well shown as “W” in Figure 2. Note that the thick-bedded chert is porous and has a distinctive log signature.

Logs of type well University Waddell field, Crane County, Texas. Location o... Available to Purchase

Published: 31 August 2006
Figure 3. Logs of type well University Waddell field, Crane County, Texas. Location of well shown as “W” in Figure 2 . Note that the thick-bedded chert is porous and has a distinctive log signature.
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Textures of cherty rocks at University Waddell field showing highly porous, thickly laminated to massive chert facies (a, b), nonporous skeletal packstone facies (c, d), and brecciated porous and nonporous chert (e, f). All samples from well 161 University Waddell. (a) Core slabs showing highly porous hydrocarbon-stained intervals and lighter gray, more tightly cemented patches (sample taken at 9032 ft [2752 m]). (b) Thin section showing abundant sponge spicule molds and incompletely silicified carbonate skeletal debris in a well-sorted skeletal packstone. Moldic dissolution porosity is up to 25%. (Sample taken at 9041 ft [2755 m].) (c) Core slab of light-colored thin-bedded to massive skeletal packstone that has local burrows and stylolites (sample taken at 8828 ft [2690 m]). (d) Thin section of skeletal packstone that has abundant coarse-grained crinoids, common brachiopods, and other skeletal grains. This facies is essentially nonporous owing to syntaxial calcite cements. (Sample taken at 9037 ft [2754 m].) (e) Core slab of oil-stained fractured/brecciated porous chert (sample taken at 8562 ft [2609 m]). (f) Core slab of brecciated, nonporous porcelaneous chert (sample taken at 8547 ft [2974 m]).

Textures of cherty rocks at University Waddell field showing highly porous,... Available to Purchase

Published: 01 January 2001
Figure 19 Textures of cherty rocks at University Waddell field showing highly porous, thickly laminated to massive chert facies (a, b), nonporous skeletal packstone facies (c, d), and brecciated porous and nonporous chert (e, f). All samples from well 161 University Waddell. (a) Core slabs
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Structure map for top of lower chert interval in University Waddell field based on correlations at the C gamma-ray log marker, the top of the major chert reservoir.

Structure map for top of lower chert interval in University Waddell field b... Available to Purchase

Published: 01 January 2001
Figure 13 Structure map for top of lower chert interval in University Waddell field based on correlations at the C gamma-ray log marker, the top of the major chert reservoir.
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Type log for the Thirtyone Formation in University Waddell field, depicting major gamma-ray markers and reservoir intervals.

Type log for the Thirtyone Formation in University Waddell field, depicting... Available to Purchase

Published: 01 January 2001
Figure 14 Type log for the Thirtyone Formation in University Waddell field, depicting major gamma-ray markers and reservoir intervals.
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Textures of cherty rocks at University Waddell field showing the finely laminated chert and limestone facies (a, b) and the disrupted laminated chert facies (c, d). All samples from well 161 University Waddell. (a) Core slab of alternating layers of gray chert, which display irregular bases and normal grading of silt-size grains, and brown lime mudstone (sample taken at 9171 ft [2795 m]). (b) Thin section of chert laminae containing silica sponge spicules and indeterminate carbonate grains in siliceous matrix (sample taken at 9172 ft [2795 m]). (c) Core slab of highly convoluted laminated chert that has abundant stylolitic dissolution seams (sample taken at 8577 ft [2614 m]). (d) Thin section of incompletely silicified chert packstone composed of silt-size to very fine grained peloids and skeletal material (sample taken at 9128 ft [2782 m]).

Textures of cherty rocks at University Waddell field showing the finely lam... Available to Purchase

Published: 01 January 2001
Figure 16 Textures of cherty rocks at University Waddell field showing the finely laminated chert and limestone facies (a, b) and the disrupted laminated chert facies (c, d). All samples from well 161 University Waddell. (a) Core slab of alternating layers of gray chert, which display irregular
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Textures of cherty rocks at University Waddell field showing nodular chert and limestone facies (a, b) and burrowed chert facies (c, d). (a) Core slab of irregular replacement chert nodules in lime mudstone matrix. Sample from 161 University Waddell at 9103 ft (2774 m). (b) Thin section of chert nodules in organic-rich lime mudstone matrix showing minor intercrystalline porosity indicated by blue epoxy along periphery of silica nodules. Sample from 161 University Waddell at 9103 ft (2774 m). (c) Core slab showing Zoophycos burrow parallel with bedding plane. Sample from 161 University Waddell at 9087 ft (2769 m). (d) Thin section of incompletely silicified, poorly sorted, silt-size to very fine-grained skeletal packstones dominated by sponge spicules. Sample from KK 10 University Waddell at 9258 ft (2821 m).

Textures of cherty rocks at University Waddell field showing nodular chert ... Available to Purchase

Published: 01 January 2001
Figure 18 Textures of cherty rocks at University Waddell field showing nodular chert and limestone facies (a, b) and burrowed chert facies (c, d). (a) Core slab of irregular replacement chert nodules in lime mudstone matrix. Sample from 161 University Waddell at 9103 ft (2774 m). (b) Thin section
Journal Article

Contrasting Styles of Reservoir Development in Proximal and Distal Chert Facies: Devonian Thirtyone Formation, Texas Available to Purchase

Stephen C. Ruppel, Roger J. Barnaby
Journal: AAPG Bulletin
Published: 01 January 2001
AAPG Bulletin (2001) 85 (1): 7–33.
DOI: https://doi.org/10.1306/8626C749-173B-11D7-8645000102C1865D
...Figure 19 Textures of cherty rocks at University Waddell field showing highly porous, thickly laminated to massive chert facies (a, b), nonporous skeletal packstone facies (c, d), and brecciated porous and nonporous chert (e, f). All samples from well 161 University Waddell. (a) Core slabs...
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View PDF for article title, Contrasting Styles of Reservoir Development in Proximal and Distal Chert Facies: Devonian Thirtyone Formation, Texas
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Distribution of reservoir facies through the primary chert reservoir section at University Waddell field.

Distribution of reservoir facies through the primary chert reservoir sectio... Available to Purchase

Published: 01 January 2001
Figure 15 Distribution of reservoir facies through the primary chert reservoir section at University Waddell field.
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Thickness and distribution of the Devonian Thirtyone Formation in west Texas showing the location of Three Bar and University Waddell fields.

Thickness and distribution of the Devonian Thirtyone Formation in west Texa... Available to Purchase

Published: 01 January 2001
Figure 2 Thickness and distribution of the Devonian Thirtyone Formation in west Texas showing the location of Three Bar and University Waddell fields.
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Model of deposition in distal Thirtyone chert reservoirs showing general morphology of turbidite channels and fans and proposed relationship to chert facies in the University Waddell field.

Model of deposition in distal Thirtyone chert reservoirs showing general mo... Available to Purchase

Published: 01 January 2001
Figure 17 Model of deposition in distal Thirtyone chert reservoirs showing general morphology of turbidite channels and fans and proposed relationship to chert facies in the University Waddell field.
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Time-structure map of Devonian Thirtyone Formation, Crane Country, Texas. Two anticlines are shown, each bounded by high-angle reverse faults (red). University Waddell field is shown by red rectangle.

Time-structure map of Devonian Thirtyone Formation, Crane Country, Texas. T... Available to Purchase

Published: 31 August 2006
Figure 1. Time-structure map of Devonian Thirtyone Formation, Crane Country, Texas. Two anticlines are shown, each bounded by high-angle reverse faults (red). University Waddell field is shown by red rectangle.
Journal Article

Developments in West Texas and Southeastern New Mexico in 1947 Available to Purchase

C. D. Cantrell, Jr., Lloyd C. Mills, Clyde W. Turner
Journal: AAPG Bulletin
Published: 01 June 1948
AAPG Bulletin (1948) 32 (6): 963–983.
DOI: https://doi.org/10.1306/3D933BAE-16B1-11D7-8645000102C1865D
... discoveries were made. Six new Ellenburger dolomite pools were found: University Waddell Ellenburger, Crane County; Jordan Ellenburger, Goldsmith Ellenburger, Yarborough-Allen, and a 2-mile Andector Ellenburger extension or new field, Ector County; Midway Lane Ellenburger, Crockett County; and Dollarhide...
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Journal Article

Rock property- and seismic-attribute analysis of a chert reservoir in the Devonian Thirty-one Formation, west Texas, U.S.A. Available to Purchase

Dongjun (Taller) Fu, E. Charlotte Sullivan, Kurt J. Marfurt
Journal: Geophysics
Published: 31 August 2006
Geophysics (2006) 71 (5): B151–B158.
DOI: https://doi.org/10.1190/1.2335636
...Figure 2. Structural geologic map of Thirtyone Formation, University Waddell field, Crane County, Texas. ...
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View PDF for article title, Rock property- and seismic-attribute analysis of a chert reservoir in the Devonian Thirty-one Formation, west Texas, U.S.A.
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Book Chapter

Rock-property and Seismic-attribute Analysis of a Chert Reservoir in the Devonian Thirty-one Formation, West Texas, U.S.A. Available to Purchase

Author(s)
Dongjun (Taller) Fu, E. Charlotte Sullivan, Kurt J. Marfurt
Book: Methods and Applications in Reservoir Geophysics
Series: Society of Exploration Geophysicists
Publisher: Society of Exploration Geophysicists
Published: 01 January 2010
EISBN: 9781560802174
... gravity deposits of carbonate rock. At many localities, these facies are difficult to predict between wells ( Ruppel and Barnaby, 2001 ). Within the survey area, faults are well mapped, particularly along the western margin University Waddell field (Figure 1 ). More important to production...
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Journal Article

McKee and Waddell Sands, Simpson Group, West Texas: GEOLOGICAL NOTES Available to Purchase

Taylor Cole, C. D. Cordry, H. A. Hemphill
Journal: AAPG Bulletin
Published: 01 February 1942
AAPG Bulletin (1942) 26 (2): 279–282.
DOI: https://doi.org/10.1306/3D93344C-16B1-11D7-8645000102C1865D
... geologist, University Lands, Midland. 3 Geologist, Gulf Oil Corporation, Fort Worth. 4 Geologist, Magnolia Petroleum Company, Midland. © 1942 American Association of Petroleum Geologists. All rights reserved 1942 American Association of Petroleum Geologists 5 Members...
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View PDF for article title, McKee and <span class="search-highlight">Waddell</span> Sands, Simpson Group, West Texas: GEOLOGICAL NOTES
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Journal Article

Developments in West Texas and Southeastern New Mexico in 1937 Available to Purchase

H. P. Bybee, Berte R. Haigh, Taylor Cole
Journal: AAPG Bulletin
Published: 01 June 1938
AAPG Bulletin (1938) 22 (6): 694–700.
DOI: https://doi.org/10.1306/3D932F92-16B1-11D7-8645000102C1865D
... with a result of 2 major and 10 minor discoveries. Several of the fields in both New Mexico and West Texas were extended. Field development accounted for 94 per cent of the drilling operations. Considerable Ordovician testing was done, but no outstanding results were obtained. The east and west boundaries...
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Journal Article

Evidence from shark teeth for a brackish Arctic Ocean in the Eocene greenhouse Available to Purchase

Sora L. Kim, Jaelyn J. Eberle, David M. Bell, Dewayne A. Fox, Aspen Padilla
Journal: Geology
Published: 01 August 2014
Geology (2014) 42 (8): 695–698.
DOI: https://doi.org/10.1130/G35675.1
... and 1M buffered CH 3 CO 2 H, respectively. CO 2 evolved from a reaction with 98% H 3 PO 4 and was analyzed on a Thermo Finnigan GasBench with a Thermo Finnigan Deltaplus XP at the University of Wyoming Stable Isotope Facility (Laramie, Wyoming, USA). (For reference materials, preparation techniques...
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Journal Article

Morphology and depositional facies of the Pennsylvanian Claytonville (Canyon lime) field, Fisher County, Texas Available to Purchase

Travis Moreland, Alexander Gonzales, Lowell Waite
Journal: AAPG Bulletin
Published: 01 March 2025
AAPG Bulletin (2025) 109 (3): 289–306.
DOI: https://doi.org/10.1306/10082423092
... ). Figure 1 The Claytonville (Canyon lime) field, located in southwestern Fisher County, was discovered on January 11, 1952, with the completion of the General Crude Oil Company No. 1 Mrs. G. T. Webb well in section 210 of H&TP RR Co. Survey, Block 3 ( Waddell, 1953 ; Galbraith, 1954...
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View PDF for article title, Morphology and depositional facies of the Pennsylvanian Claytonville (Canyon lime) <span class="search-highlight">field</span>, Fisher County, Texas
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