Transition from deep-marine lower-slope erosional channels to proximal basin-floor stacked channel–levée–overbank deposits, and syn-sedimentary growth structures, Middle Eocene Banastón System, Ainsa Basin, Spanish Pyrenees

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Title
Transition from deep-marine lower-slope erosional channels to proximal basin-floor stacked channel–levée–overbank deposits, and syn-sedimentary growth structures, Middle Eocene Banastón System, Ainsa Basin, Spanish Pyrenees
Authors
Keywords
Eocene, Deep-marine, Submarine channels, Syn-sedimentary tectonics
Journal
EARTH-SCIENCE REVIEWS
Volume 144, Issue -, Pages 23-46
Publisher
Elsevier BV
Online
2014-12-31
DOI
10.1016/j.earscirev.2014.11.015

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