Validation of accumulation rates in Teluk Banten (Indonesia) from commonly applied 210Pb models, using the 1883 Krakatau tephra as time marker.

W. Boer, G.D. van den Bergh, H. de Haas, H.C. de Stigter, R. Gieles, T.C.E. van Weering

    Research output: Contribution to JournalArticleAcademicpeer-review

    Abstract

    Teluk Banten is a tropical shallow marine embayment on the north coast of Java, close to the Krakatau volcanic complex. The tsunami generated by the 1883 Krakatau eruption resulted in the deposition of a tsunamite tephra layer on the bottom of Teluk Banten. The Krakatau Event Layer has been used as a time marker to validate
    Original languageEnglish
    Pages (from-to)263-277
    JournalMarine Geology
    Volume227
    DOIs
    Publication statusPublished - 2006

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