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Asset Overview
Fluvial strata, Eocene South-Pyrenean Foreland Basin, Aragón. The two main sandstone-bodies (7-8 m thick thick each) are mostly point bar deposits with epsilon cross-bedding resulting from lateral acretion. Minor portions of the sandstone bodies are channel-fill deposits and chute cut-off deposits. The fine-grained units in between sandstone bodies are floodplain deposits.
