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Tuesday, April 28, 2020 | History

2 edition of Atoka formation on the north side of the McAlester Basin found in the catalog.

Atoka formation on the north side of the McAlester Basin

Jack Gordon Blythe

Atoka formation on the north side of the McAlester Basin

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  • 16 Currently reading

Published by Oklahoma Geological Survey in Norman, OK .
Written in English

    Subjects:
  • Geology, Stratigraphic -- Pennsylvanian.,
  • Geology -- Oklahoma.

  • Edition Notes

    Statementby Jack G. Blythe.
    SeriesCircular (Oklahoma Geological Survey) -- 47
    ContributionsOklahoma Geological Survey.
    Classifications
    LC ClassificationsQE"153"A3"no.47
    The Physical Object
    Pagination74 p. :
    Number of Pages74
    ID Numbers
    Open LibraryOL20620162M

    Carbonate rocks of Desmoinesian (Middle Pennsylvanian Strawn) age form hydrocarbon reservoirs in many oil and gas fields in the Permian Basin of west Texas (Fig. A) and southeastern New Mexico. The reservoirs occur in stratigraphic and stratigraphic-structural combination traps, and are predominantly algal and coralgal buildups (“reefs Cited by: 7. Mississippian Stratigraphy of Manitoba. H. R. McCabe. Gypsumville Hayes River inch indicated interbanded interbedded isopach Jurassic Knee Lake light grey limestone lithology Lodgepole Formation Lower Lodgepole Lyleton Manitoba map-area massive matrix medium Mission Canyon Mississippian Mississippian strata mottled North Dakota occur. Crow-Flies-High (32MZ1), a historic Hidatsa village in the Garrison Reservoir area, North Dakota (River Basin Surveys papers) [Malouf, Carling I] on *FREE* shipping on qualifying offers. Crow-Flies-High (32MZ1), a historic Hidatsa village in the Garrison Reservoir area, North Dakota (River Basin Surveys papers)Author: Carling I Malouf.


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Atoka formation on the north side of the McAlester Basin by Jack Gordon Blythe Download PDF EPUB FB2

COVID Resources. Reliable information about the coronavirus (COVID) is available from the World Health Organization (current situation, international travel).Numerous and frequently-updated resource results are available from this ’s WebJunction has pulled together information and resources to assist library staff as they consider how to handle.

Lynn Mountain Formation (Early Pennsylvanian) at surface, covers 9 % of this area. McALESTER TEXARKANA- Shale, gray to tan, with many fine- to coarse-grained, quartzose, micaceous sandstone with many bottom markings; top eroded; thickness, 3, to 7, feet or more; unconformable upon Goddard, Delaware Creek, Woodford, and older beds that are exposed.

First published use in Pittsburg Co, OK, in the Arkoma basin. Probably named for the town of McAlester. No type locality designated. Occurs in the McAlester coal district in the McAlester quadrangle, and in the Lehigh coal district in the Atoka and Colgate quadrangles.

Discussion of Atoka formation on north side of McAlester basin. Formation passes northward into a platform facies, thins, and is overlapped by Desmoinesian rocks.

Facies changes and thinning of section north of Arkansas River made it unwise to attempt perfect identification of the rapidly thinning shelf-facies section with member as described.

Posts about Atoka Formation written by argeology. The Geologic Road Guide to Arkansas State High a Geotour of the Southern Arkoma Basin Fold Belt and Related Ouachita Mountain Tectonic Zones by Drs.

Atoka formation on the north side of the McAlester Basin book Cohoon (Emeritus), Jason Patton (Associate), and Victor Vere (Emeritus), Professors of Geology at Arkansas Tech University, is now available for download. Savanna Formation, Arkoma basin, Oklahoma, from outcrops and surface and subsurface gamma-ray profiles: OGS Oklahoma Geology Notes, v.

62, p. Andrews, R.D.,Bypassed gas production in a recently Atoka formation on the north side of the McAlester Basin book Hartshorne gasFile Size: KB.

December Bibliography of Arkoma Basin and Northeast Oklahoma Shelf Brian Atoka formation on the north side of the McAlester Basin book.

Cardott Oklahoma Geological Survey Alsalhi, R.A.,Atoka Formation sequence stratigraphy in Arkoma Basin, Haskell and Blythe, J.G.,Atoka Formation on the north side of the McAlester basin: OGS Circu 74 p.

Bowker, K., and J. Seale,The. Stratigraphy and Depositional Environment of the Middle Atoka Formation, Central Arkoma Basin, Western Arkansas A thesis submitted in partial fulfillment of the requirements for the degree Atoka formation on the north side of the McAlester Basin book Master of Science in Geology by Yueyang Wang China University of Petroleum Bachelor of Engineering in Resource Exploration, December Author: Yueyang Wang.

The atoka formation in north-central Arkansas [Stone, Charles G] on *FREE* shipping on qualifying offers. The atoka formation in north-central ArkansasAuthor: Charles G Stone. Sedimentology. The Atoka Formation is a sequence of marine sandstones, siltstones, and shales, and may be as thick at 25, feet in the Ouachita Mountains.

The formation is conformable with the Bloyd Shale in the Boston Mountains and the Johns Valley Formation in the Ouachita Mountains. Paleofauna Trace Fossils. Conostichus; C. arkansanus ReferencesCountry: United States. Book Stores in Mcalester on See reviews, photos, directions, phone numbers and more for the best Book Stores in Mcalester, OK.

Corporate Headquarters. Express Lane McAlester, OK PH: FAX: are rare. The Choctaw fault separates the strata of the coal basin from the more intensely deformed strata of the Ouachita Mountains, which lie to the south.

Along that fault strata on the south side have been thrust northward over younger strata on the north by: 1. History. Atoka was founded by the Choctaw Indians in the s, and named for Captain Atoka, a leader of the Choctaw Nation and the signer of the Treaty of Dancing Rabbit Creek, which began the process of re-locating the Choctaw people from Mississippi to Oklahoma in The name "Atoka" is derived from the Choctaw word hitoka (or hetoka), which means "ball ground" in County: Atoka.

TABLE 1. Division of the Atoka Formation in Van Buren and Lavaca quadrangles, Arkansas and Oklahoma._____ A15 2. Estimated original reserves of coal in the Arkansas part of Van Buren and Lavaca quadrangles, Arkansas and Oklahoma.

_____ 27 : Boyd Raymond Haley, Thomas Andrews Hendricks. InHolleyman co-founded and serves as CEO of Basin Environmental & Safety Technologies and Basin Transportation. He is also a Registered Professional Engineer in the State of Oklahoma (P.E.

Read Full Bio. Arkansas Academy of Science Proceedings,32 Stratigraphy ofthe Lower AtokaFormation, Crawford County, Arkansas JOHN G.

CHAPMAN,JAMES P. THORNTON and DOY Department of Geology, University of Arkansas, Fayettevi lie ABSTRACT The Atoka Formation (Pennsylvanian) ofnorthwestern Arkansas is acomplex succession of. Atoka Sands (Pregnant Shale or Davis Sand) This north Texas zone is often called the “Pregnant Shale” because of its characteristic shape on down-hole electric logs.

The zone is a poor performer in general, with the median wells producing MMCFG, and the average well producing about MMCFG.

Evolution from Passive Margin to Foreland Basin: The Atoka Formation of the Arkoma Basin, South‐Central U.S.A. Chapter (PDF Available) May Author: David Houseknecht. Geology. Collins, et al published a detailed description of the interval in (in Depositional Environments, Petrology and Fractures of the Atoka Davis Sandtone: A Low-permeability Gas-bearing Sandstone of the Fort Worth Basin, North Central Texas {Transactions of the Southwest Section of American Association of Petroleum Geologists Annual Convention, Publication.

High and lowstand deposition. Source: Dr. Scholle Exploratory drilling continues in the Delaware Basin, with El Capitan and the Guadalupe Mountains in the background.

Source: Thomas Smith About million years ago, the Permian Basin, which now covers a large area of central USA, was situated along the western margin of Pangaea, about 10° north of the paleo-equator.

The Atoka Formation along the southwestern margin of the Arkoma basin in Coal and Pontotoc Counties, Oklahoma, is predominantly a mudstone unit interbedded with thin (less than 30 ft), horizontally stratified, sandstones and rare, thin, sandy limestones.

Atoka Formation on the North Side of the McAlester Basin by Jack G. Blythe [Oklahoma Geological Survey, Circu ] bound edition, inscribed to VerWiebe and signed by author. Box 3: FF 5: Bulletin of the American Association of Petroleum Geologists [Vol.

6, Number 3, May-June, ] Box 3: FF 6. The Prairie Grove and Bloyd sedimentary basin received sandy sediments from the north and northeast.

The dissimilar rock types, including limestone, conglomerate, phosphorite, and coal, within the Morrow indicate a complex depositional history. The Atoka Formation is the only part of the Atoka Series present in this area.

The Permian Basin formed as an area of rapid Mississippian-Pennsylvanian subsidence in the foreland of the Ouachita fold belt. It is one of the largest sedimentary basins in the U.S., and has oil and gas production from several reservoirs from Permian through Ordovician in age. The term "Wolfberry" was coined initially to indicate commingled.

The clastic wedge, the Atoka Formation, is synorogenic and up to km thick in the southern part of the basin and was deposited mainly by E-W-trending submarine fans in a neritic to bathyal environment (Houseknecht,).

Although the Atoka sediments comprise more than three fourths of the entire Pennsylvanian. Jackfork formation. There has been much controversy on age of Jackfork formation. A Morrow (lower Pennsylvanian) fauna has been found by Honess at base of his "Upper Jackfork" sandstone, which he correlates with Atoka formation.

Miser therefore excludes "Upper Jackfork" of Honess from Jackfork formation and maps it as Atoka on State map. The Booch Sandstones (McAlester Formation, Krebs Group), Arkoma Basin, Oklahoma – Outcrops to Well Logs: An Introduction to Oklahoma Fluvial Reservoirs* Neil H.

Suneson1 Search and Discovery Article # () Posted Septem *Adapted from presentation to Tulsa Geological Society, September 8, Circular Chesterian and Morrowan rocks in the McAlester basin of Oklahoma, by Richard B.

Laudon. November 30 pages, 14 figures. Circular Atoka formation on the north side of the McAlester Basin, by Jack G.

Blythe. July 74 pages, 24 figures. 17 Circular Cenozoic geology of northern Roger Mills County, Oklahoma, by David B. Atoka specializes in unconventional Natural Gas resources, such as Coal Bed Methane, Fractured Shale, and Tight Gas sands.

Our services extend from Desorption and Adsorption, Mudlogging, and Rock Properties Determination, Exploration to Exploitation Planning, Interpretation to Production Optimization and Operations.

the Barnett formation of the Permian and Ft. Worth Basins and the Rancheria Formation of southern New Mexico outcrops.

These rocks accumulated by autochthonous hemipelagic sedimentation and allochthonous mass gravity transport in low energy, below wave base, dysaerobic conditions in a platform marginal deep water basin formed on the southern. McAlester is a city in and the county seat of Pittsburg County, Oklahoma, United States.

The population at the census, a percent increase f at the census, making it the largest city in the Choctaw Nation of Oklahoma, followed by town gets its name from James Jackson McAlester, an early white settler and businessman County: Pittsburg.

Rheic Ocean closure recorded in the deepwater Atoka Formation through Sandstone and Mudrock Provenance Studies.

Problems to be addressed: Despite decades of study and proposed contradictory plate tectonic models, the tectonostratigraphic evolution of Ouachita Trough is not well understood along the southern margin of Laurentia.

The county line between Pittsburg and Atoka counties runs approximately feet south of the main gate that leads into the facility. Pasted below is a brief news article snippet about the facility. Article: Tenaska and Kiowa Power Partners Announce Construction Of 1,MW Oklahoma Electric Generating Facility.

Abstract: Sequence Stratigraphy and Depositional Dynamics, Atoka Formation (Middle Pennsylvanian), Southern Ozarks, Northeastern Oklahoma and Northwestern Arkansas. Deposition of the Atoka Formation (Middle Pennsylvanian) in the northern Arkoma Basin and adjacent shelf is characterized by an alternation of sandstones and shales.

View Kehler__Morrilton from GEOL at Louisiana State University. Geological Society of America Centennial Field GuideSouthCentral Section.

STRUCTURAL GEOMETRY OF THE FRONTAL OUACHITAS-ARKOMA BASIN TRANSITION ZONE IN WESTERN ARKANSAS By DONALD JORDAN YEZERSKI within the accommodation zone between the Choctaw Fault and Ross Creek Fault in north-central Scott County, western Arkansas.

Oklahoma and coincides with the formation of the laterally File Size: 8MB. Atokan Sandstone Stratigraphic Gas Play by Mitchell E.

Henry and Timothy C. Hester Much like Morrow Group strata, Atoka Group strata are oriented in a broad band that occupies most of the province, except that part along the northeastern and southwestern edges of.

This thesis represents a surface and subsurface geologic study of the stratigraphy, including sedimentology and petrography, of the McAlester Formation (Booch) Sandstones.

The area covered includes Haskell, Muskogee, and Mcintosh Counties with parts of Okmulgee and Pittsburg Counties, : Clinton Randall Bissell. The Red Cave Formation of the Texas Panhandle by R G Rogers 12 other sections not shown. Other editions - View all. Oil and Gas Fields of the Texas and Oklahoma Panhandles: Symposium Snippet view - Common terms and phrases.

Amarillo Anadarko basin ANALYSIS OF PAY anhydrite AREAL EXTENT arkosic Atoka Average thickness bbls Beaver. Oil and gas well pdf parameters, including peakmonthly production (PMP), peak-consecutive-twelve month production (PYP), and cumulative production (CP), are tested as tools to quantify and understand the heterogeneity of reservoirs in fields where current monthly production is 10 percent or less of PMP.

Variation coefficients, defined as VC= (F5-F95)/F50. The Southern Oklahoma Download pdf () is a relatively well explored (mature), petroleum-rich, province of Paleozoic age located in south-central Oklahoma.

The province is bounded to the northeast by the Ada Dome, to the east by the Ouachita Mountains, to the south by the Waurika-Muenster Uplift, and to the west and northwest by the Anadarko Size: KB.11 Township 13 North, Range 4 West of the Indian Meridian in Ebook County, Oklahoma. 12 Kiamichi Basin Hydrologic Model – means the surface water hydrologic model for 13 the Kiamichi Basin, inclusive of tributaries thereto, that the State of Oklahoma, the Chickasaw.