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Sedimentary Facies Structure And Palynology Of The Lower And Middle Members Of The Atoka Formation Central Arkansas
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Book Synopsis Sedimentary Facies, Structure, and Palynology of the Lower and Middle Members of the Atoka Formation, Central Arkansas by : Harold Edward Quinn
Download or read book Sedimentary Facies, Structure, and Palynology of the Lower and Middle Members of the Atoka Formation, Central Arkansas written by Harold Edward Quinn and published by . This book was released on 1986 with total page 314 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Sequence Stratigraphy and Depositional Dynamics, Basal Atoka Formation (Orr-Patterson Members), Middle Pennsylvanian, Arkoma Basin, Central Arkansas by : Jamie Ann Woolsey
Download or read book Sequence Stratigraphy and Depositional Dynamics, Basal Atoka Formation (Orr-Patterson Members), Middle Pennsylvanian, Arkoma Basin, Central Arkansas written by Jamie Ann Woolsey and published by . This book was released on 2007 with total page 280 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis The Shelf to Basin Transition and Tectonostratigraphy of the Atoka Formation (lower Pennsylvanian) in the Arkoma Basin, Northwest Arkansas by : Travis Gibson White
Download or read book The Shelf to Basin Transition and Tectonostratigraphy of the Atoka Formation (lower Pennsylvanian) in the Arkoma Basin, Northwest Arkansas written by Travis Gibson White and published by . This book was released on 2019 with total page 178 pages. Available in PDF, EPUB and Kindle. Book excerpt: The east-to-west oriented Arkoma Basin is a peripheral foreland basin or depositional trough that developed during the Carboniferous Period. This formation covers an aerial extent of approximately 33,800 square miles and spans from west-central Arkansas into southeastern Oklahoma (McGilvery, Manger, and Zachry, 2016; Perry, 1995). The Atoka Formation, deposited during the early Pennsylvanian, is the largest Paleozoic formation by aerial extent in the state of Arkansas and is located within and comprises the bulk of Arkoma Basin sediments (McFarland, 2004; Nance, 2018). This formation has been informally divided into three divisions, the lower, middle, and upper, based on their stratigraphic response to differing tectonic processes. A tectonostratigraphic interpretation was made for each division of the Atoka Formation using high resolution cross sections; correlated using well log, seismic, and surface data. Five condensed regional transects were constructed that aided in the development of a cross section "grid" meant to represent the deep marine to shallow marine depositional hinge lines. Each of the three Atoka divisions have a different dominant depositional force. The Lower Atoka deposition was dominated by eustasy, and with sediment supply from the start of Arkoma Basin tectonics, the middle division was dominated by tectonic subsidence and the upper was dominated by sediment supply. The transition between the Atoka divisions and the magnitude of migration between each deep marine hinge line indicates the progradation of the Upper Atoka depositional cycles occurred more rapidly than the retrogradation of the Middle Atoka. The maximum flooding of the formation occurred within the Middle Atoka's uppermost informal member, the Morris Member. The Lower Atoka was deposited on an extensive tectonically stable structural platform, which is supported by no lithostratigraphic transition to deep marine deposits within this project's study area. The deep marine deposition is characterized by shales encapsulating tumultuously distributed and isolated sandstone complexes. These sandstone complexes are not correlated to the shallow marine sandstones by anything but a condensed geologic timeline.
Book Synopsis Masters Theses in the Pure and Applied Sciences by : Wade H. Shafer
Download or read book Masters Theses in the Pure and Applied Sciences written by Wade H. Shafer and published by Springer. This book was released on 1988-10-31 with total page 400 pages. Available in PDF, EPUB and Kindle. Book excerpt: Masters Theses in the Pure and Applied Sciences was first conceived, published, and disseminated by the Center for Information and Numerical Data Analysis and Synthesis (CINDAS) * at Purdue University in 1957, starting its coverage of theses with the academic year 1955. Beginning with Volume 13, the printing and dissemination phases of the activity were transferred to University Microfilms/Xerox of Ann Arbor, Michigan, with the thougtit that such an arrangement would be more beneficial to the academic and general scientific and technical community. After five years of this joint undertaking we had concluded that it was in the interest of all con cerned if the printing and distribution of the volumes were handled by an interna tional publishing house to assure improved service and broader dissemination. Hence, starting with Volume 18, Masters Theses in the Pure and Applied Sciences has been disseminated on a worldwide basis by Plenum Publishing Cor poration of New York, and in the same year the coverage was broadened to include Canadian universities. All back issues can also be ordered from Plenum. We have reported in Volume 31 (thesis year 1986) a total of 11 ,480 theses titles trom 24 Canadian and 182 United States universities. We are sure that this broader base tor these titles reported will greatly enhance the value ot this important annual reterence work. While Volume 31 reports theses submitted in 1986, on occasion, certain univer sities do re port theses submitted in previousyears but not reported at the time.
Book Synopsis Sedimentary and Igneous Rocks of the Ouachita Mountains of Arkansas by : Charles Gomer Stone
Download or read book Sedimentary and Igneous Rocks of the Ouachita Mountains of Arkansas written by Charles Gomer Stone and published by . This book was released on 1986 with total page 280 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Bibliography and Index of Geology by :
Download or read book Bibliography and Index of Geology written by and published by . This book was released on 1990 with total page 1516 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis A Guidebook to the Atoka Formation in Arkansas by : William V. Bush
Download or read book A Guidebook to the Atoka Formation in Arkansas written by William V. Bush and published by . This book was released on 1978 with total page 70 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Structural Cross Sections and Subsurface Maps of the Atoka Formation in the Northern Arkoma Basin, Western and Northwestern Arkansas by : David Lewis Nance
Download or read book Structural Cross Sections and Subsurface Maps of the Atoka Formation in the Northern Arkoma Basin, Western and Northwestern Arkansas written by David Lewis Nance and published by . This book was released on 2018 with total page 210 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Arkoma Basin is one of several peripheral foreland basins situated on the front of the Ouachita orogenic fold and thrust belt. The transition from the foredeep to the Ozark Plateaus is a short one in terms of latitude. The Atoka Formation in Arkansas comprises the bulk of the sediments in the Arkoma Basin. Three divisions of the Atoka Formation have been informally assigned as the Upper, Middle, and Lower based on differences in sedimentary response to tectonic processes that occurred during the formation and subsidence of the Arkoma Basin. In the Arkansas portion of the Arkoma Basin, the lower Atoka marks the onset of tectonic subsidence in between the Mulberry and the Cass Fault systems and displays a maximum of almost 1,000 feet of thickening in the study area. The middle Atoka in the same area gains a maximum of 4,000 feet of sediment. The upper Atoka achieves a maximum thickness of 1,800 feet. Entrapment of hydrocarbons within the Atoka Formation in the Arkoma Basin has led many oil and gas companies to penetrate and log the formation with electric, gamma ray and other mechanical logs while exploring for natural gas. This study uses these raster logs to provide a variety of maps and cross sections that illustrate the coastal systems of the lower and upper Atoka Formation and aid in the interpretation of the sedimentary response of the three Atoka divisions with respect to structural timing and sedimentology. With the subsurface maps and cross sections, a more synthesized version of the Atoka Formation in the northern Arkoma Basin of western version is produced.
Book Synopsis Reconstruction of Depositional Environments of the Lower Carpenter and Glassy Intervals of the Middle Atoka Formation (Pennsylvanian), in the Arkoma Basic, Arkansas by : Melody Rae Hacker
Download or read book Reconstruction of Depositional Environments of the Lower Carpenter and Glassy Intervals of the Middle Atoka Formation (Pennsylvanian), in the Arkoma Basic, Arkansas written by Melody Rae Hacker and published by . This book was released on 2002 with total page 144 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Stratigraphy and Depositional Environment of the Middle Atoka Formation, Central Arkoma Basin, Western Arkansas by : Yueyang Wang
Download or read book Stratigraphy and Depositional Environment of the Middle Atoka Formation, Central Arkoma Basin, Western Arkansas written by Yueyang Wang and published by . This book was released on 2016 with total page 126 pages. Available in PDF, EPUB and Kindle. Book excerpt: Wire line logs are widely used in analysis of the subsurface stratigraphy of the middle Atoka Formation, Central Arkoma Basin, Western Arkansas. SP log, Gamma ray log, resistivity log and conductivity log provide valuable information to construct cross sections. The middle Atoka formation is composed of a succession of shale and sandstone alternations with thickness reaching approximately 3000 feet in the study area. It contains several sandstone units which include Morris, Tackett, Areci, Bynum, Casey and Dunn "A" separated by shale intervals. The purpose of this study is to identify these units and predict sequence stratigraphy and depositional environment by constructing cross-sections, observing wireline logs and associating previous research. Several isopach maps are made, explaining the development of sandstone in target units such as Tackett and Casey. The sequence stratigraphy of the middle Atoka formation is mainly composed of transgressive systems tracts and part of a highstands systems tract. The intervals indicate successive sea-level cycles associated transgression and regression from shallow marine to shoreface. The middle Atoka formation has been proved as a significant exploration target since 1950's. In order to understand geologic setting and find potential reservoirs within the Arkoma basin, it is vital to comprehend the sequence development and depositional environment of the intervals within the middle Atoka.
Book Synopsis Characterization of the Lower Atoka Formation, Arkoma Basin, Central Arkansas by : Kelly R. LaGrange
Download or read book Characterization of the Lower Atoka Formation, Arkoma Basin, Central Arkansas written by Kelly R. LaGrange and published by . This book was released on 2002 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Depositional Dynamics and Stratigraphic Correlation, Basal Atoka Formation (Spiro-Foster Members), Middle Pennsylvanian, Arkoma Basin, Eastern Oklahoma by : Zachary W. Mullen
Download or read book Depositional Dynamics and Stratigraphic Correlation, Basal Atoka Formation (Spiro-Foster Members), Middle Pennsylvanian, Arkoma Basin, Eastern Oklahoma written by Zachary W. Mullen and published by . This book was released on 2009 with total page 156 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Depositional Environment and Petrology of the Lower Member of the Pennsylvanian Atoka Formation, Ouachita Mountains, Arkansas and Oklahoma by : Anthony Ross Grafton Sprague
Download or read book Depositional Environment and Petrology of the Lower Member of the Pennsylvanian Atoka Formation, Ouachita Mountains, Arkansas and Oklahoma written by Anthony Ross Grafton Sprague and published by . This book was released on 1985 with total page 553 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Stratigraphic and Structural Evolution of the Ouachita Mountains and Arkoma Basin, Southeastern Oklahoma and West-central Arkansas by :
Download or read book Stratigraphic and Structural Evolution of the Ouachita Mountains and Arkoma Basin, Southeastern Oklahoma and West-central Arkansas written by and published by . This book was released on 2005 with total page 140 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis The Atoka Formation in North-central Arkansas by : Charles Gomer Stone
Download or read book The Atoka Formation in North-central Arkansas written by Charles Gomer Stone and published by . This book was released on 1968 with total page 11 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Depositional Systems of the Lower Atoka Formation in the Arkoma Basin, Arkansas by : Jay S. Johnston
Download or read book Depositional Systems of the Lower Atoka Formation in the Arkoma Basin, Arkansas written by Jay S. Johnston and published by . This book was released on 1982 with total page 232 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis A Subsurface Stratigraphic Study of the Middle Atoka, Sebastian County, Arkansas by : Sara Beth Sutton
Download or read book A Subsurface Stratigraphic Study of the Middle Atoka, Sebastian County, Arkansas written by Sara Beth Sutton and published by . This book was released on 2012 with total page 120 pages. Available in PDF, EPUB and Kindle. Book excerpt: Raster log images were analyzed to study the subsurface stratigraphy of the Middle Atoka in the Arkoma Basin of the western portion (Sebastian County) of Arkansas. The most significant sandstone units of the Middle Atoka in this area were determined to be two generally coarsening-upward sequences in the lower portion of the formation. Based on lithologic correlations, these two units were determined to be the informally named Casey and Freiburg members of the Middle Atoka. Thickness information based on picked tops was used to create isopach maps of the units of interest. The log signatures and geometry of the sand bodies indicate that they were deposited in a deltaic system that prograded across this portion of this basin. Distributary-mouth bar deposits dominate the Casey member, and are occasionally overlain by localized channel deposits. Avulsion of the delta lobe possibly occurred, and a new lobe then began to prograde, depositing the sediments that formed the Freiburg. This unit is also dominated by distributary-mouth bar deposits.
