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Denmar Formation

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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1985
AAPG Bulletin (1985) 69 (9): 1449.
...E. M. Sullivan; D. A. Textoris Abstract: The Denmar Formation of Randolph County is a package of interbedded marine carbonates and siliciclastics deposited on a broad subsiding carbonate platform. Seven major microfacies are recognized: terrigenous siltstone, dolomitized micrite, pelmicrite...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1950
AAPG Bulletin (1950) 34 (5): 882–922.
...Dana Wells ABSTRACT The lower middle Mississippian (lower Greenbrier age) of southeastern West Virginia is composed of the Hillsdale and Denmar (new) formations of the Meramecian series. These formations are predominantly calcarenites and calcilutites deposited in a transgressing sea along...
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FAUNULES FROM <b>DENMAR</b> <b>FORMATION</b> OF WEST VIRGINIA
Published: 01 May 1950
TABLE II FAUNULES FROM DENMAR FORMATION OF WEST VIRGINIA
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1985
AAPG Bulletin (1985) 69 (2): 318.
...Cindy A. Yeilding; Eileen M. Sullivan; Daniel A. Textoris; John M. Dennison ABSTRACT The Greenbrier Group of eastern West Virginia consists of marine carbonates interbedded and mixed with siliciclastics that were deposited on a shallow shelf in the Late Mississippian. The Denmar Formation...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1950
AAPG Bulletin (1950) 34 (9): 1910–1912.
... stratigraphic detail little additional comment is necessary. These things are factual and must be accepted as such. The author, unfortunately, has yielded to the common urge for stratigraphic reorganization and hasty generalization that seems to plague many young writers. He introduces a “Denmarformation...
Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2003
DOI: 10.2110/pec.03.78.0035
EISBN: 9781565763340
... by fourth-order sequences that are only a few meters to 15 meters thick, which is an order of magnitude thinner than those of the proximal foreland. Regional disconformities marked by paleosols, caliche, micro-karsting, brecciation, tepee formation, or sharp contacts between limestone and the overlying...
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Series: AAPG Hedberg Series, AAPG Hedberg Series
Published: 01 January 2008
DOI: 10.1306/13131057H33327
EISBN: 9781629810324
... of a shale or an evaporite formation is replaced by a capillary soft seal caused by a transition from low-permeability downdip rocks to high-permeability updip rocks. Hydrodynamic trapping, an explanation that has been cited for many years, is not required. Instead, the gas is just sitting in a pancake...
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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2003
DOI: 10.2110/pec.03.78.0011
EISBN: 9781565763340
... the top of each sequence. Major biostratigraphic markers include Acrocyathus in the Hillsdale Formation, the last appearance of Platycrinites penicillus at the top of the Denmar Formation, the first appearance of Talarocrinus in the Pickaway Formation, as well as the conodont zones (Fig. 3...
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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2001
DOI: 10.2110/pec.01.71.0167
EISBN: 9781565761933
... of eolianites in Kentucky are intensely brecciated, and are draped by thin green lithoclastic mudrock. Quartzose carbonate eolianites are abundant in the Lower Chesterian (Upper Mississippian) Ste. Genevieve and Paoli Formations of the Illinois and western Appalachian Basins and the age-equivalent Denmar...
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