2016
DOI: 10.1130/abs/2016am-286365
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Depostional Environment and Sequence Stratigraphy of the Pennsylvanian Morrowan and Atokan Intervals at the Farnworth Unit, Ochiltree County Texas

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Cited by 7 publications
(11 citation statements)
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“…Tectonic activities including the creation of folds and faults of the Ouachita-fold belt, Cimarron arch, Apishapa, Nemaha and Amarillo Wichita upliftment, and Arkoma basin subsidence [23,24] are of the Wichita orogeny (caused by the North-American plate colliding with the South-American plate through the Morrowan to Des Moinesian period). Others interpret it to be caused by the generation of stress through the southwestern Laurentia margin [23,24]. Past studies interpret Morrow sands in north-west Anadarko deposit to be fluvial [19,[25][26][27][28].…”
Section: The Farnsworth Unit-lithostratigraphic and Geological Settingsmentioning
confidence: 99%
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“…Tectonic activities including the creation of folds and faults of the Ouachita-fold belt, Cimarron arch, Apishapa, Nemaha and Amarillo Wichita upliftment, and Arkoma basin subsidence [23,24] are of the Wichita orogeny (caused by the North-American plate colliding with the South-American plate through the Morrowan to Des Moinesian period). Others interpret it to be caused by the generation of stress through the southwestern Laurentia margin [23,24]. Past studies interpret Morrow sands in north-west Anadarko deposit to be fluvial [19,[25][26][27][28].…”
Section: The Farnsworth Unit-lithostratigraphic and Geological Settingsmentioning
confidence: 99%
“…However, the authors of [29,30] suggested incised valley infill through regression and further transgression. The depositional environment for the Atokan Thirteen Finger Limestone, in contrast to Morrowan sands and shales, was estuarine to marginal marine with coals, and mudstones intercalated with limestones forming the major lithology [23,30].…”
Section: The Farnsworth Unit-lithostratigraphic and Geological Settingsmentioning
confidence: 99%
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“…The target formation, Morrow B, is highly heterogeneous due in part to dispersed clay deposited during its diagenetic evolution. 31,32 Several studies have shown the unpredictable impacts of clay content on the Biot-Gassmann workflow results. [33][34][35] Consequently, the appropriate implementation of Biot Gassmann requires the development of a relationship between the properties of the rocks' composite grains and the rock frame, aptly expressed through the Biot poroelastic coefficient (Eqn 7), 36,37 K fr = (1 − α) K s (7) This study benefits from a site-specific Krief rock physics model.…”
Section: Seismic Velocity: Impact Of Fluid Substitutionmentioning
confidence: 99%
“…An additional assumption is that the acoustic waves propagate through the formation at low frequencies such that the seismic waves do not trigger pressure disequilibration within the pore spaces. The target formation, Morrow B, is highly heterogeneous due in part to dispersed clay deposited during its diagenetic evolution 31,32 . Several studies have shown the unpredictable impacts of clay content on the Biot‐Gassmann workflow results 33–35 .…”
Section: Theorymentioning
confidence: 99%