Current studentsExisting staffContact us
 

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

Simple item page
dc.contributor.authorBourget, J.
dc.contributor.authorZaragosi, S.
dc.contributor.authorEllouz-Zimmermann, S.
dc.contributor.authorDucassou, E.
dc.contributor.authorPrins, M.
dc.contributor.authorGarlan, T.
dc.contributor.authorLanfumey, V.
dc.contributor.authorSchneider, J.
dc.contributor.authorRouillard, P.
dc.contributor.authorGiraudeau, J.
dc.date.issued2010
dc.description.statementofresponsibilityJ. Bourget, S. Zaragosi, S. Ellouz-Zimmermann, E. Ducassou, M.A. Prins, T. Garlan, V. Lanfumey, J.-L. Schneider, P. Rouillard, J. Giraudeau
dc.identifier.citationMarine Geology, 2010; 274(1-4):187-208
dc.identifier.doi10.1016/j.margeo.2010.04.005
dc.identifier.issn0025-3227
dc.identifier.urihttp://hdl.handle.net/2440/65125
dc.language.isoen
dc.publisherElsevier Science BV
dc.rights© 2010 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.margeo.2010.04.005
dc.subjectturbidite system
dc.subjectgravity flow
dc.subjectactive margin
dc.subjecteustasy
dc.subjectclimate
dc.subjecttectonics
dc.subjectearthquake recurrence
dc.subjectsource-to-sink
dc.titleHighstand vs. lowstand turbidite system growth in the Makran active margin: Imprints of high-frequency external controls on sediment delivery mechanisms to deep water systems
dc.typeJournal article
pubs.publication-statusPublished

Files

Collections

Australian School of Petroleum publications