Sedimentology and geomorphology of the modern epsilon cross-stratified point bar deposits in the Athabasca upper delta plain ...
Bibliography: p. 103-116. ... : Epsilon cross-stratification (ECS) has been observed in many ancient channel point bar deposits. Investigation of ECS in modern tidal and estuarine systems has been limited in scale and/or detail of investigation. ECS has been documented to exist in only one fluvial s...
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| Format: | Master Thesis |
| Language: | English |
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University of Calgary
1984
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| Online Access: | https://dx.doi.org/10.11575/prism/23984 https://prism.ucalgary.ca/handle/1880/22954 |
| Summary: | Bibliography: p. 103-116. ... : Epsilon cross-stratification (ECS) has been observed in many ancient channel point bar deposits. Investigation of ECS in modern tidal and estuarine systems has been limited in scale and/or detail of investigation. ECS has been documented to exist in only one fluvial system. The search for a modern large scale analogue led to the investigation of the point bar deposits in the fluvially-dominated, freshwater Athabasca Delta in northeastern Alberta. The channels of the upper delta plain are muddy fine-grained and highly sinuous in character with fluctuating discharge. The investigation concentrated on the determination of the overall sedimentological trends in terms of grain size, thickness, variability, continuity and geometry. Proximal to distal transects along point bars were investigated primarily by (1) coring the subaqueous sediments down to a maximum depth of 8.9 m and (2) trenching the subaerial sediments parallel and perpendicular to flow. Two scales of cross-stratification were apparent: (1) very ... |
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