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Dufeu M. (1999). Métabolisme des polyamines et amines aromatiques chez la Brassicaceae Pringlea antiscorbutica:viabilité des graines, germination et émergence de la jeune plante en fonction du régime thermique..
Abstract: Mémoire de DEA GAPV, Université de Rennes I
Programme: 136
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Raymond C.A. & Giret A. (1997). Southern Ocean Evolution: Introduction. Terra antarctica, 3(2), 650–652.
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Trouvilliez A. (2010). Modélisation et quantification de, la neige soufflée en Antarctique, . Bachelor's thesis, , .
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Bureau Central De Magnetisme Terrestre. (1995). Réseaux magnétiques de répétition, France Métropolitaine 1987, Terres Australes et Antarctiques Françaises 1981-1989, Afrique de l'Ouest 1983-1986. Bulletin, 5.
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Gusmeroli Alessio, Pettit Erin C, Kennedy Joseph H, Ritz Catherine, . (2012). The crystal fabric of ice from full-waveform borehole sonic logging
. J. Geophys. Res., 117(F3), F03021–.
Abstract: In an ice sheet, a preferred crystal orientation fabric affects deformation rates because ice crystals are strongly anisotropic: shear along the basal plane is significantly easier than shear perpendicular to the basal plane. The effect of fabric can be as important as temperature in defining deformation rates. Fabric is typically measured using analysis of thin sections under the microscope with co-polarized light. Due to the time-consuming and destructive nature of these measurements, however, it is difficult to capture the spatial variation in fabric necessary for evincing ice sheet flow patterns. Because an ice crystal is similarly elastically anisotropic, the speed of elastic waves through ice can be used as a proxy for quantify anisotropy. We use borehole sonic logging measurements and thin section data from Dome C, East Antarctica to define the relations between apparent fabric and borehole measured elastic speeds (compressional VP and vertically polarized shear VSV). These relations, valid for single maximum fabrics, allow in-situ, depth-continuous fabric estimates of unimodal fabric strength from borehole sonic logging. We describe the single maximum fabric using a1: the largest eigenvalue of the second-order orientation tensor. For ice at -16C and a1 in the 0.7-1 range the relations are VP = 248 a13.7 + 3755 m s-1 and VSV = -210a17.3 + 1968 m s-1.
Keywords: Ice anisotropy, borehole sonic logging, ice crystal fabric, 0726 Cryosphere: Ice sheets, 0915 Exploration Geophysics: Downhole methods, 0935 Exploration Geophysics: Seismic methods (3025, 7294),
Programme: 902
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Guinet C., Jouventin P. & Weimerskirch H. (1999). Recent population change of the southern elephant seal at îles Crozet and Kerguelen: the end of the decrease? Antarct. Sci., 11(2), 193–197.
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Iyemori T., Araki T., Kamei T. & Takeda M. (1997). Mid-latitude geomagnetic indices ASY and SYM. Data Analysis Center for Geomagnetic and Space Magnetism, 7.
Abstract: Publication annuelle du Data Analysis Center for Geomagnetic and Space Magnetism
Programme: 139
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Cherel Y., Verdon C. & Ridoux V. (1993). Seasonal importance of oceanic myctophids in king penguin diet at Crozet Islands. Polar Biol., 13, 355–357.
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Roult Genevieve, Montagner Jean-Paul, Romanowicz Barbara, Cara Michel, Rouland Daniel, Pillet Robert, Karczewski Jean-Francois, Rivera Luis, Stutzmann Eleonore, Maggi Alessia, the GEOSCOPE team, . (2010). The GEOSCOPE Program: Progress and Challenges during the Past 30 Years
. Seismological Research Letters, 81(3), 427–452.
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Giret A. (1993). Les étapes magmatiques de l'édification des îles Kerguelen, océan Indien. Memoires de la societe geologique de france, 163, 273–282.
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