Lateral and vertical juxtaposition of matrix-rich and matrix-poor lithologies caused by particle settling in mixed mud-sand deep-marine sediment suspensions
Author:
Affiliation:
1. Department of Earth and Environmental Sciences; University of Ottawa; Ottawa ON K1N 6N5 Canada
2. Husky Energy Inc.; Calgary AB T2P-1H5 Canada
3. Northwest Territories Geological Survey; Yellowknife NT X1A-2L9 Canada
Funder
Husky Energy Graduate Fellowships
Natural Sciences and Engineering Research Council of Canada
Windermere Consortium
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12523/fullpdf
Reference57 articles.
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2. Anatomy of turbidites and linked debrites based on long distance (120 × 30 km) bed correlation, Marnoso Arenacea Formation, Northern Apennines, Italy;Amy;Sedimentology,2006
3. An experimental investigation of sand-mud suspension settling behaviour: implications for bimodal mud contents of submarine flow deposits;Amy;Sedimentology,2006
4. Angus , K. 2016 Lateral trends in deep-marine slope and basin-floor matrix-rich beds, Neoproterozoic Windermere Supergroup, British Columbia, Canada 152
5. Geological Association of Canada;Arnott,2010
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