Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/65125
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Type: Journal article
Title: 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
Author: Bourget, J.
Zaragosi, S.
Ellouz-Zimmermann, S.
Ducassou, E.
Prins, M.
Garlan, T.
Lanfumey, V.
Schneider, J.
Rouillard, P.
Giraudeau, J.
Citation: Marine Geology, 2010; 274(1-4):187-208
Publisher: Elsevier Science BV
Issue Date: 2010
ISSN: 0025-3227
Statement of
Responsibility: 
J. Bourget, S. Zaragosi, S. Ellouz-Zimmermann, E. Ducassou, M.A. Prins, T. Garlan, V. Lanfumey, J.-L. Schneider, P. Rouillard, J. Giraudeau
Keywords: turbidite system
gravity flow
active margin
eustasy
climate
tectonics
earthquake recurrence
source-to-sink
Rights: © 2010 Elsevier B.V. All rights reserved.
DOI: 10.1016/j.margeo.2010.04.005
Published version: http://dx.doi.org/10.1016/j.margeo.2010.04.005
Appears in Collections:Aurora harvest
Australian School of Petroleum publications

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