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Walshville Channel

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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1980
AAPG Bulletin (1980) 64 (8): 1283.
... the Walshville Channel (interpreted as a major distributary channel deposit in the study area). Facies recognition and interpretation of depositional environments are based upon lithology, sedimentary structures, vertical and lateral relations, geometry, and paleoecology as well as organic matter content...
Journal Article
Published: 01 November 1987
Journal of Sedimentary Research (1987) 57 (6): 1060–1067.
... thick, which thin away from the Walshville channel (interpreted as a major channel deposit), and local pods or lenses which occur farther from the channel. Facies recognition and interpretation of depositional environments are based on paleoecology, lithology, sedimentary structures, vertical...
Journal Article
Published: 01 September 1979
Journal of Sedimentary Research (1979) 49 (3): 1005–1013.
...M. J. Edwards; R. L. Langenheim; W. J. Nelson; C. Ledvina Abstract The Energy Shale Member, an argillaceous wedge associated with the Walshville Channel and Herrin (No. 6) Coal Member, consists of a lower dark-gray shale unit and an upper light-gray shale unit in the Orient No. 6 Mine...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1983
AAPG Bulletin (1983) 67 (9): 1454.
... of coarse-grained sediments from the nearby Walshville channel were deposited as crevasse splays. The bay-fill deposits include a nonmarine and a brackish-marine facies; the latter has higher sulfur and boron contents and a sparse marine fauna. Both bay-fill facies are faintly laminated gray shales...
Image
Map of a portion of Franklin County, IL, showing thick wedges of Energy Sha...
Published: 01 January 2000
Fig. 4. Map of a portion of Franklin County, IL, showing thick wedges of Energy Shale and areas of erosionally modified roof, called transitional roof. All known coal ball sites are also plotted. The position of the Walshville channel is identified by partly or fully missing Herrin Coal
Journal Article
Published: 01 January 2000
Journal of the Geological Society (2000) 157 (1): 221–228.
...Fig. 4. Map of a portion of Franklin County, IL, showing thick wedges of Energy Shale and areas of erosionally modified roof, called transitional roof. All known coal ball sites are also plotted. The position of the Walshville channel is identified by partly or fully missing Herrin Coal...
FIGURES | View All (8)
Journal Article
Published: 01 February 1999
Journal of the Geological Society (1999) 156 (1): 137–148.
.... Assemblage (1) consists of channel sandstone bodies, containing beds of calcrete breccia, cordaite logs (up to 3 m long), and coniferopsid wood charcoal. This assemblage records upland coniferopsid forest fires which altered basin hydrology and promoted flooding in downstream floodplain rivers. Assemblage (2...
Journal Article
Journal: PALAIOS
Published: 01 June 2003
PALAIOS (2003) 18 (3): 197–211.
... , 1988 , 1994 ). The other occupied adjacent nutrient-rich, wetland clastic substrates such as floodbasins and channel levees ( Gastaldo et al., 1995 ), and was dominated by the same plant groups as those in the peat mires, but with distinctly different dominance-diversity patterns ( DiMichele et al...
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