Ichnology of fine-grained mixed carbonate-siliciclastic turbidites, Wood River Formation, Pennsylvanian-Permian, south-central Idaho

In south-central Idaho, the Wood River Formation (Pennsylvanian-Permian) contains a stratigraphic megacycle over 2000 m thick that is composed of fine-grained mixed carbonate-siliciclastic turbidites. Complete and partial (Bouma) turbidite structural sequences in these rocks are arranged in upward t...

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Veröffentlicht in:	Palaios 1991-06, Vol.6 (3), p.291-301
Hauptverfasser:	Burton, Bradford Robert, Link, Paul Karl
Format:	Artikel
Sprache:	eng
Schlagworte:	580000 - Geosciences biogenic structures Blaine County Idaho Boulder Mountains Bouma sequence CARBONATE ROCKS Carboniferous CARBONIFEROUS PERIOD Chondrites DEVELOPED COUNTRIES DIMENSIONS Earth sciences Earth, ocean, space Exact sciences and technology FEDERAL REGION X FOSSILS GEOLOGIC AGES GEOLOGIC FORMATIONS GEOLOGIC HISTORY GEOLOGIC STRUCTURES Geological facies Geological surveys GEOLOGY GEOSCIENCES Ichnofabric and Ichnofacies IDAHO Invertebrate paleontology lebensspuren NORTH AMERICA Oxygen PALEONTOLOGY Paleozoic PALEOZOIC ERA Pennsylvanian Permian PERMIAN PERIOD River basins ROCKS sed rocks, sediments SEDIMENTARY BASINS sedimentary petrology SEDIMENTARY ROCKS sedimentary structures Sediments Silts STRATIGRAPHY THICKNESS Tissue oxygenation Trace fossils turbidite turbidity current structures United States upper Paleozoic USA Wood River Formation
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