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

doi:10.1016/j.margeo.2005.12.002

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 Journal › Article › Academic › peer-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 language	English
Pages (from-to)	263-277
Journal	Marine Geology
Volume	227
DOIs	https://doi.org/10.1016/j.margeo.2005.12.002
Publication status	Published - 2006

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10.1016/j.margeo.2005.12.002

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

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",

author = "W. Boer and {van den Bergh}, G.D. and {de Haas}, H. and {de Stigter}, H.C. and R. Gieles and {van Weering}, T.C.E.",

year = "2006",

doi = "10.1016/j.margeo.2005.12.002",

language = "English",

volume = "227",

pages = "263--277",

journal = "Marine Geology",

issn = "0025-3227",

publisher = "Elsevier B.V.",

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TY - JOUR

T1 - Validation of accumulation rates in Teluk Banten (Indonesia) from commonly applied 210Pb models, using the 1883 Krakatau tephra as time marker.

AU - Boer, W.

AU - van den Bergh, G.D.

AU - de Haas, H.

AU - de Stigter, H.C.

AU - Gieles, R.

AU - van Weering, T.C.E.

PY - 2006

Y1 - 2006

N2 - 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

AB - 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

U2 - 10.1016/j.margeo.2005.12.002

DO - 10.1016/j.margeo.2005.12.002

M3 - Article

SN - 0025-3227

VL - 227

SP - 263

EP - 277

JO - Marine Geology

JF - Marine Geology

ER -

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

Abstract

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