Sedimentology and depositional architecture of tufas deposited in stepped fluvial systems of changing slope: Lessons from the Quaternary Añamaza valley (Iberian Range, Spain)

The Pleistocene and Holocene tufas of the Añamaza valley (stepped build‐ups, up to 70 m thick, along the valley) consist of several depositional stages separated by erosional surfaces. Eight associations of tufa and related carbonate facies, plus minor polygenic detrital facies, represent the proces...

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Veröffentlicht in:Sedimentology 2014-01, Vol.61 (1), p.133-171
Hauptverfasser: Arenas, Concha, Vázquez-Urbez, Marta, Pardo, Gonzalo, Sancho, Carlos
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Sprache:eng
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