Fluvial facies changes at the last interglacial-glacial transition, when and how did they occur? An example from a fluvial sequence in Twente, Eastern Netherlands.

J. van Huissteden, S.J.P. Bohncke

    Research output: Contribution to ConferenceAbstractOther research output

    Original languageEnglish
    Publication statusPublished - 1998

    Bibliographical note

    Proceedings title: INQUA-SEQS symposium, Kerkrade.

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