Article ID Journal Published Year Pages File Type
4690562 Sedimentary Geology 2008 16 Pages PDF
Abstract
The Bajo Barreal Formation differs from the classic model of syn-eruptive and inter-eruptive depositional conditions in the presence of a braided fluvial pattern during inter-eruptive periods, at least at one locality. This braided fluvial pattern is attributed to the high input of fine-grained pyroclastic material that composes the loessic sediments.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
Mechanisms of aggradation in fluvial systems influenced by explosive volcanism: An example from the Upper Cretaceous Bajo Barreal Formation, San Jorge Basin, Argentina
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