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Hindsville Formation

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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1968
AAPG Bulletin (1968) 52 (2): 282–294.
...David E. Ogren ABSTRACT Recommendations are made for a revision of terminology and correlations in the Upper Mississippian strata of northern Arkansas. The terms “Mayes Group” and “Hindsville Formation” are applied as they are used in northeast Oklahoma, the term “Ruddell Shale” is recommended...
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Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/13632144M1163785
EISBN: 9781629812854
... is grouped with the Hindsville Formation in the upper Mayes cycle. Present in both the lower and upper Mayes cycles are high-frequency shallowing-upward cycles bounded by flooding surfaces. Evaluating the distribution of facies and stratigraphic surfaces within a framework of multiple orders of depositional...
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Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/13632142M1163785
EISBN: 9781629812854
... Chesterian conodont fauna. The lower two subzones within Biozone 4 correspond to the Lindsey Bridge (Biozone 4L) and Ordnance Plant (Biozone 4M) members of the Pryor Creek Formation, whereas the upper subzone consists of the Hindsville Formation (Biozone 4U). Documentation of conodont taxa and recognition...
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Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/136321482158M1163788
EISBN: 9781629812854
... by the Chesterian-aged Hindsville Formation ( Huffman, 1958 ; Figure 2 ). The east (Wall 3) and west (Wall 2) walls depict dip-oriented depositional profiles, whereas the southern wall (Wall 1) shows a strike-oriented profile. Blasting conducted in the last decade produced vertical outcrop faces characterized...
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Journal Article
Published: 01 February 2022
Journal of Paleontology (2022) 96 (S87): 1–38.
..., lay in demonstrating that their non-P 1 elements (i.e., their P 2 , M, S 0 , S 1 , S 2 , and S 3/4 elements) were also identical. Thus, we re-collected the type locality and type stratum of S . commutatus , the Hindsville Formation at locality 4 in Oklahoma, from which we recovered a few P 2 , M...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1933
AAPG Bulletin (1933) 17 (12): 1436–1445.
... of Mississippian age, successively become the surface formations. The Chester series is made up of the Carterville of Missouri, which is probably equivalent in part to the Batesville sandstone, the Fayetteville shale, and the Hindsville limestone of northern Arkansas. H. S. McQueen of the Missouri Geological...
FIGURES
Image
Lochriea commutata  (Branson and Mehl, 1941) (Branson and Mehl,  1941b ) P ...
Published: 01 February 2022
designated as paralectotypes and given new numbers) by von Bitter and Norby ( 1994a , fig. 2.6–2.9). Hindsville Formation, locality 4, Oklahoma, USA. Length = 0.91 mm. ( 11–18 ) P 1 s elements ( 14, 16–18 ) and P 1 d elements ( 11, ?12, 13, 15 ), upper views of approximate ontogenetic growth series from
Journal Article
Journal: AAPG Bulletin
Published: 01 September 2014
AAPG Bulletin (2014) 98 (9): 1739–1759.
..., and the sequence boundary grades into a correlative conformity downslope to the south and east ( Handford and Manger, 1993 ; Handford, 1995 ). The overlying Upper Mississippian succession includes the Moorefield Formation, Batesville Sandstone (including the Hindsville Limestone Member), Fayetteville Shale...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1959
AAPG Bulletin (1959) 43 (11): 2541–2574.
... are those between the top of the Precambrian and the base of the Simpson. These beds together comprise the Timbered Hills and Arbuckle groups as recognized in the Arbuckle Mountain region. The Timbered Hills group ( Decker, 1933 ) consists of the Reagan sandstone and the overlying Honey Creek formation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1930
AAPG Bulletin (1930) 14 (2): 121–138.
..., with a thickness somewhat greater south of Lincoln. West of Fayetteville the formation in most places rests unconformably on the Boone, but farther east the Batesville sandstone, with the Hindsville limestone member locally present, occupies the interval between the Boone and the Fayetteville shale. Locally...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1974
AAPG Bulletin (1974) 58 (2): 269–282.
... correlations that elucidate regional biostratigraphic relations in the area of investigation. The Early Mississippian Caballero and biohermal Lake Valley Formations are restricted to the northern part of the area of investigation. The maximum development of the Middle and Late Mississippian Las Cruces...
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Journal Article
Journal: Geosphere
Published: 12 January 2018
Geosphere (2018) 14 (2): 710–730.
... fractures that would otherwise be aliased from on-scanner camera imagery. The fracture system developed within the exposures of the Mississippian Boone Formation, an outcrop analog for age-equivalent reservoir objectives in Mississippi Lime hydrocarbon play, was characterized using conventional and virtual...
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Journal Article
Published: 01 June 2004
Environmental Geosciences (2004) 11 (2): 99–111.
... ). The Fayetteville Formation is considered to rest conformably on the Batesville Sandstone (and Hindsville Member; Figure 3 ), although at places, it unconformably overlies the Boone chert ( Handford, 1986 ). Samples for this study were collected from the trangressive marine facies near the base of the formation...
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Series: GCSSEPM
Published: 01 December 2009
DOI: 10.5724/gcs.09.29.0209
EISBN: 978-0-9836096-1-2
... interbeds of limestone and siliceous, cherty material. The Fayetteville Shale overlies formations of the Mayes Group in Arkansas, the Batesville Sandstone in northeastern Arkansas, and the Hindsville Formation in northwestern Arkansas ( Ogren, 1968 ). In outcrop, the Fayetteville is overlain by the Pitkin...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1941
AAPG Bulletin (1941) 25 (9): 1619–1705.
...-Cambrian units in the Wichitas was determined by Hoffman (5). These rocks are overlain, unconformably, by upper Cambrian and Permian sediments. Merritt and Ham (6) have recently discovered another pre-Cambrian sedimentary formation, composed of zeolite, opal, calcite, and dolomite, exposed near Tepee...
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Series: AAPG Memoir
Published: 01 January 2003
DOI: 10.1306/M77973
EISBN: 9781629810041
... are elongate in a vertical dimension. Although isolated fenestrae occur in sedimentary carbonates, it is more common to find many in close association. Fenestrae are generally associated with microbial mats and result from shrinkage, gas formation, organic decay, trapping of air through swash-zone wave action...
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Series: GSA Field Guide
Published: 01 January 2010
DOI: 10.1130/2010.0017(05)
EISBN: 9780813756172
..., the highest unit of the Mississippian succession exposed in these road cuts. Overlying Mississippian units, the Burlington-Keokuk limestones (undivided), including the Short Creek Oolite Member of the Keokuk Limestone, Warsaw, Hindsville, and Batesville formations are exposed farther south along Highway 65...
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Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/13632140M1163784
EISBN: 9781629812854
..., Elsey Formation, Burlington–Keokuk Limestone, and Short Creek Oolite Member. The terms “Boone Group” and “Boone Formation” are not recognized in southwest Missouri. Meramecian-age strata are represented by the Warsaw Formation, and the Chesterian-age strata consist of the Hindsville and Batesville...
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Series: AAPG Memoir
Published: 01 January 2003
DOI: 10.1306/M77973
EISBN: 9781629810041
...). The presence of micritic matrix or oolitic coatings can inhibit the formation of such overgrowths. PHOTO SCALES AND ABBREVIATIONS ARE EXPLAINED IN THE BOOKʼS INTRODUCTION Diagrammatic view of typical echinoids This diagram (adapted from Moore et al., 1952 ) emphasizes some of the features...
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