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Highstand vs. lowstand turbidite system growth in the Makran active margin: Imprints of high-frequency external controls on sediment delivery mechanisms to deep water systems
  • J. Bourget, S. Zaragosi, S. Ellouz-Zimmermann, E. Ducassou, M.A. Prins, T. Garlan, V. Lanfumey, J.-L. Schneider, P. Rouillard, J. Giraudeau
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한국지질자원연구원

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2013-12-19

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논문

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Data type 해외논문
저널명 Highstand vs. lowstand turbidite system growth in the Makran active margin: Imprints of high-frequency external controls on sediment delivery mechanisms to deep water systems
Document number J0127401015
Author J. Bourget, S. Zaragosi, S. Ellouz-Zimmermann, E. Ducassou, M.A. Prins, T. Garlan, V. Lanfumey, J.-L. Schneider, P. Rouillard, J. Giraudeau
???year??? 2010
Vol/No 274/01
Page 187 ~ 208
Keyword turbidite system; gravity flow; active margin; eustasy; climate; tectonics; earthquake recurrence; source-to-sink
Source 원문링크

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J. Bourget, S. Zaragosi, S. Ellouz-Zimmermann, E. Ducassou, M.A. Prins, T. Garlan, V. Lanfumey, J.-L. Schneider, P. Rouillard, J. Giraudeau. (2010). Highstand vs. lowstand turbidite system growth in the Makran active margin: Imprints of high-frequency external controls on sediment delivery mechanisms to deep water systems.