Cyclic sedimentation in the Eocene Allenby Formation of south-central British Columbia and the origin of the Princeton chert fossil beds

Canadian Journal of Earth Sciences

Volumn 48, Issue 1, 2011, Pages 25-43

  Mustoe, George E ^a  

^a WESTERN WASHINGTON UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BOUNDARY FAULTS; BRITISH COLUMBIA; CYCLIC DEPOSITION; CYCLIC SEDIMENTATION; DEBRIS FLOWS; DISSOLVED OXYGEN LEVELS; DISSOLVED SILICA; FLOOD PLAINS; FLUVIAL SEDIMENT; GEOCHEMICAL CHANGES; HYDROLOGIC CHANGES; IN-SITU; METAVOLCANIC ROCKS; OPEN WATER; ORGANIC MATTER; SEISMIC ACTIVITY; SOUTH-CENTRAL BRITISH COLUMBIA; SUBBITUMINOUS COAL; TOPOGRAPHIC CHANGES; UPPER TRIASSIC; VOLCANIC DEBRIS; VOLCANIC FLOWS;

BITUMINOUS COAL; COAL DEPOSITS; COAL INDUSTRY; DEBRIS; DEPOSITS; DISSOLUTION; DISSOLVED OXYGEN; GROUNDWATER; HYDRAULICS; LAKES; METAMORPHIC ROCKS; SANDSTONE; SEDIMENTOLOGY; SILICA; SOLVENTS; STREAM FLOW; VOLCANOES; WETLANDS;

CARBONACEOUS SHALE;

ALLUVIAL DEPOSIT; CHERT; CONGLOMERATE; CYCLIC SEDIMENTATION; DEBRIS FLOW; DIAGENESIS; DISSOLVED OXYGEN; EOCENE; FOSSIL ASSEMBLAGE; LAHAR; METAVOLCANIC ROCK; TEPHRA; TRIASSIC; TUFF; VOLCANIC ERUPTION;

BRITISH COLUMBIA; CANADA; PRINCETON [BRITISH COLUMBIA]; SIMILKAMEEN RIVER;

EID: 78951474317     PISSN: 00084077     EISSN: 14803313     Source Type: Journal    
DOI: 10.1139/E10-085     Document Type: Article

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