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Nadine Ellouz-Zimmermann - Publications

Affiliations: 
Université de Bordeaux, Talence, Nouvelle-Aquitaine, France 
Area:
, Sedimentology, Gulf of Oman, Turbidite system, East-African margin, Gravity flow,, Sedimentary transfer, External forcings, Late Quaternary, Monsoon
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5 high-probability publications. We are testing a new system for linking publications to authors. You can help! If you notice any inaccuracies, please sign in and mark papers as correct or incorrect matches. If you identify any major omissions or other inaccuracies in the publication list, please let us know.

Year Citation  Score
2011 Bourget J, Zaragosi S, Ellouz-Zimmermann N, Mouchot N, Garlan T, Schneider JL, Lanfumey V, Lallemant S. Turbidite system architecture and sedimentary processes along topographically complex slopes: The Makran convergent margin Sedimentology. 58: 376-406. DOI: 10.1111/J.1365-3091.2010.01168.X  0.567
2011 Caley T, Malaizé B, Zaragosi S, Rossignol L, Bourget J, Eynaud F, Martinez P, Giraudeau J, Charlier K, Ellouz-Zimmermann N. New Arabian Sea records help decipher orbital timing of Indo-Asian monsoon Earth and Planetary Science Letters. 308: 433-444. DOI: 10.1016/J.Epsl.2011.06.019  0.663
2010 Bourget J, Zaragosi S, Mulder T, Schneider JL, Garlan T, Van Toer A, Mas V, Ellouz-Zimmermann N. Hyperpycnal-fed turbidite lobe architecture and recent sedimentary processes: A case study from the Al Batha turbidite system, Oman margin Sedimentary Geology. 229: 144-159. DOI: 10.1016/J.Sedgeo.2009.03.009  0.698
2010 Mouchot N, Loncke L, Mahieux G, Bourget J, Lallemant S, Ellouz-Zimmermann N, Leturmy P. Recent sedimentary processes along the Makran trench (Makran active margin, off Pakistan) Marine Geology. 271: 17-31. DOI: 10.1016/J.Margeo.2010.01.006  0.7
2008 Bourget J, Zaragosi S, Garlan T, Gabelotaud I, Guyomard P, Dennielou B, Ellouz-Zimmermann N, Schneider JL. Discovery of a giant deep-sea valley in the Indian Ocean, off eastern Africa: The Tanzania channel Marine Geology. 255: 179-185. DOI: 10.1016/J.Margeo.2008.09.002  0.682
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