José María Hernández Gómez, Victoriano Pujalte Navarro, Sergio Robles Orozco
Four diferents types of rizoliths have been recognized within the alluvio-lacustrine deposits that made up the Aguilar Fm. On the base of their macroscopic and microscopic features and of the sedimentology of the facies association in which they occurred, a genetic model is proposed for each of them.
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