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Une phase de sédimentation alluviale au Préboréal initial dans la vallées de l'Escaut (Nord de la France)

Abstract : in Fresnes-sur-Escaut, a partial cross-section of the Schelde's right bank alluviums is marked out, under the holocene silt, peat and calcarous tufa deposits, by a thick sandy bedded deposit with vegetal remains (3 m), of which the higher half is dated from the Lateglacial-Holocene transition or the early Holocene (10040 ± 50 BP). It could be a quick sedimentary accumulation (favored by local factors) m response to the major climatic oscillation pointing out the begining of the Holocene.
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https://hal-inrap.archives-ouvertes.fr/hal-01489295
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Laurent Deschodt. Une phase de sédimentation alluviale au Préboréal initial dans la vallées de l'Escaut (Nord de la France). Quaternaire, AFEQ-CNF INQUA, 2002, 13 (2), pp.149 - 152. ⟨10.3406/quate.2002.2188⟩. ⟨hal-01489295⟩

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