Spatial variation in the sedimentary architecture of a dryland fluvial system

Ancient dryland terminal fluvial systems are often recognized within the rock record for having a progressive downstream decrease in the size and amalgamation of channel elements and systematic downstream increase in sheet and overbank elements, alongside the downstream decrease in grain size that i...

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Veröffentlicht in:	Sedimentology 2021-10, Vol.68 (6), p.2887-2917
Hauptverfasser:	Priddy, Charlotte L., Clarke, Stuart M., Fielding, Christopher
Format:	Artikel
Sprache:	eng
Schlagworte:	Aeolian Amalgamation Approximation Arid lands Arid zones Aridity Complexity Distance distributive fluvial systems Downstream effects dryland ephemeral–fluvial Fluvial sedimentation Fluvial sediments Grain size Jurassic Kayenta Formation Particle size Sediments Spatial distribution Spatial variations Thickness Trends
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