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TitleCambrian wave-dominated tidal-flat deposits, central Wisconsin, USA
 
AuthorMacNaughton, R BORCID logo; Hagadorn, J W; Dott, R H, Jr.
SourceSedimentology 2018 p. 1-30, https://doi.org/10.1111/sed.12546
Year2018
Alt SeriesEarth Sciences Sector, Contribution Series 20090316
PublisherWiley
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf; html; tif
AreaWisconsin; United States of America
Lat/Long WENS -93.0000 -87.0000 47.0000 42.5000
Subjectsregional geology; sedimentology; paleontology; stratigraphy; depositional environment; coastal environment; tidal flats; channels; mud flats; tides; bedrock geology; lithology; sedimentary rocks; arenites; sandstones; mudstones; siltstones; sedimentary structures; facies; ichnofacies; fossils; ichnofossils; lithofacies; Elk Mound Group; Wonewoc Formation; Eau Claire Formation; Mount Simon Formation; Cruziana; Molluscs; Furongian; Miaolingian; Trends; Phanerozoic; Paleozoic; Cambrian
Illustrationslocation maps; cross-sections; lithologic sections; rose diagrams; photographs; sketches; geoscientific sketch maps; tables; plots; block diagrams
ProgramPeople Support
Released2018 10 18
AbstractIn central Wisconsin, Cambrian strata of the Elk Mound Group record deposition on open-coast, wave-dominated tidal flats. Mature, medium-grained quartz arenite is dominated by parallel-bedding with upper-flow regime parallel-lamination, deposited during high-energy storms that also produced three-dimensional bedforms on the flats. Abundant wave ripples were produced as storms waned or during fair weather, in water depths
GEOSCAN ID254289

 
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