Search Results - "Buret, Christophe"

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  1. 1
    Present-day principal horizontal stress orientations in the Kumano forearc basin of the southwest Japan subduction zone determined from IODP NanTroSEIZE drilling Site C0009

    Present-day principal horizontal stress orientations in the Kumano forearc basin of the southwest Japan subduction zone determined from IODP NanTroSEIZE drilling Site C0009 by Lin, Weiren, Doan, Mai-Linh, Moore, J. Casey, McNeill, Lisa, Byrne, Timothy B., Ito, Takatoshi, Saffer, Demian, Conin, Marianne, Kinoshita, Masataka, Sanada, Yoshinori, Moe, Kyaw Thu, Araki, Eiichiro, Tobin, Harold, Boutt, David, Kano, Yasuyuki, Hayman, Nicholas W., Flemings, Peter, Huftile, Gary J., Cukur, Deniz, Buret, Christophe, Schleicher, Anja M., Efimenko, Natalia, Kawabata, Kuniyo, Buchs, David M., Jiang, Shijun, Kameo, Koji, Horiguchi, Keika, Wiersberg, Thomas, Kopf, Achim, Kitada, Kazuya, Eguchi, Nobuhisa, Toczko, Sean, Takahashi, Kyoma, Kido, Yukari

    Published in Geophysical research letters (01-07-2010)
    “…A 1.6 km riser borehole was drilled at site C0009 of the NanTroSEIZE, in the center of the Kumano forearc basin, as a landward extension of previous drilling…”
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  2. 2
    Primary or secondary distal volcaniclastic turbidites: how to make the distinction? An example from the Miocene of New Zealand (Mahia Peninsula, North Island)

    Primary or secondary distal volcaniclastic turbidites: how to make the distinction? An example from the Miocene of New Zealand (Mahia Peninsula, North Island) by Schneider, Jean-Luc, Le Ruyet, Anthony, Chanier, Frank, Buret, Christophe, Ferrière, Jacky, Proust, Jean-Noël, Rosseel, Jean-Baptiste

    Published in Sedimentary geology (01-12-2001)
    “…Miocene marine volcaniclastic deposits occur in Mahia Peninsula (North Island, New Zealand) and were sedimented in a forearc setting related to the Hikurangi…”
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  3. 3
    La Mamora, charnière entre la Meseta et le Rif: son importance dans l'évolution géodynamique postpaléozoïque du Maroc / The Mamora Plain, a hinge between the Meseta and the Rif. Its importance in the post-Paleozoic geodynamic evolution of Morocco

    La Mamora, charnière entre la Meseta et le Rif: son importance dans l'évolution géodynamique postpaléozoïque du Maroc / The Mamora Plain, a hinge between the Meseta and the Rif. Its importance in the post-Paleozoic geodynamic evolution of Morocco by Zouhri, Lahcen, Lamouroux, Christian, Buret, Christophe

    Published in Geodinamica acta (01-12-2001)
    “…The Mamora area (Morocco) is located in the northern part of the Meseta and the southern part of Rharb. The recent formations (Mesozoic to Quaternary) lie…”
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  4. 4
    Tubular structures of northern Wairarapa (New Zeland) as possible examples of ancient fluid expulsion in an accretionary prism : evidence from field and petrographical observations

    Tubular structures of northern Wairarapa (New Zeland) as possible examples of ancient fluid expulsion in an accretionary prism : evidence from field and petrographical observations by Ledésert, Béatrice, Buret, Christophe, Chanier, Franck, Ferrière, Jacky, Recourt, Philippe

    Published in Journal of the Geological Society (2003)
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  5. 5
    La Mamora, charnière entre la Meseta et le Rif : son importance dans l’évolution géodynamique post-paléozoïque du Maroc

    La Mamora, charnière entre la Meseta et le Rif : son importance dans l’évolution géodynamique post-paléozoïque du Maroc by Zouhri, Lahcen, Lamouroux, Christian, Buret, Christophe

    Published in Geodinamica acta (2001)
    “…La Mamora (Maroc), bordure méridionale du bassin du Rharb, comporte un ensemble de dépôts récents recouvrant un substratum essentiellement paléozoïque…”
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