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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This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 14 Life Below Water

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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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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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