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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/69134
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dc.contributor.authorBourget, Julienen
dc.contributor.authorZaragosi, Sebastienen
dc.contributor.authorEllouz-Zimmermann, Nadineen
dc.contributor.authorMouchot, Nicolasen
dc.contributor.authorGarlan, Thierryen
dc.contributor.authorSchneider, Jean-Lucen
dc.contributor.authorLanfumey, Valentineen
dc.contributor.authorLallemant, Siegfrieden
dc.date.issued2011en
dc.identifier.citationSedimentology, 2011; 58(2):376-406en
dc.identifier.issn0037-0746en
dc.identifier.urihttp://hdl.handle.net/2440/69134-
dc.description.statementofresponsibilityJulien Bourget, Sebastien Zaragosi, Nadine Ellouz-Zimmermann, Nicolas Mouchot, Thierry Garlan, Jean-Luc Schneider, Valentine Lanfumey and Sigfried Lallemanten
dc.language.isoenen
dc.publisherBlackwell Publishing Ltden
dc.rights© 2010 The Authors. Journal compilation © 2010 International Association of Sedimentologistsen
dc.subjectActive margin; gravity flow; Gulf of Oman; hydraulic jump; plunge pool; slope break deposits; submarine slope; turbidite system.en
dc.titleTurbidite system architecture and sedimentary processes along topographically complex slopes: the Makran convergent marginen
dc.typeJournal articleen
dc.contributor.schoolAustralian School of Petroleumen
dc.identifier.doi10.1111/j.1365-3091.2010.01168.xen
Appears in Collections:Australian School of Petroleum publications

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