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Paleosol stratigraphy, a technique commonly applied in basin–margin settings to depict cyclic alluvial architecture on time scales of 10–100ky, can be consistent with regional accommodation trends at even higher temporal resolution (1–10ky), having strong implications for the sequence stratigraphy of late Quaternary, non-marine deposits. Three closely-spaced late Pleistocene paleosols (P1–P3), dating...
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