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Amalvict M. et al. (2005). Absolute Gravity measurements in the Indian Ocean.
Abstract: Scientific Assembly of the International Associati
Programme: 337
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Amalvict M. et al. (2003). Measurements in Antarctica: a review.
Abstract: Colloque du GDR G2, Paris
Programme: 337
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Amalvict M. et al. 2005. (2005). DORIS in Antarctica.
Abstract: Scientific Assembly of the International Associati
Programme: 337
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Amalvict M., Bouin M.-N., Hinderer J. & Luck B. (2003). Results of the first absolute gravity measurements at Crozet Island, and repetition at Kerguelen and La Réunion Islands.
Abstract: 9th Symposium on Antarctic Earth Sciences, Potsdam
Programme: 337
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Amalvict M., Hinderer J., & Rozsa S. (2006). Crustal vertical motion along a profile crossing the Rhine graben from the Vosges to the Black Forest Mountains: Results from absolute gravity, GPS and levelling observations. Journal of geodynamics, 41, 358–368.
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Amalvict M., Hinderer J., Makinen J., Rosat S. & Rogister Y. (2004). Long-term and seasonal gravity changes and their relation to crustal deformation and hydrology. Journal of geodynamics, 38, 343–353.
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Amalvict M., Willis P., Wöppelmann G., Ivins E., Bouin MN, Testut L., & Hinderer J.,. (2009). Stability of the East Antarctic station Dumont d’Urville from long-term geodetic observations and geophysical model. Polar research, 28(2), 193–202.
Abstract: Geodetic measurements of the vertical crustal displacement collocated with absolute gravity changes provide a discriminatory measurement of present-day glacial changes, versus more deeply seated rock motions caused by glacial isostatic adjustment (GIA). At the East Antarctic station of Dumont d'Urville, we compare the displacements derived from continuous DORIS (1993.0–2006.0) and Global Positioning System (GPS) (1999.0–2005.7) data, and observed changes in absolute gravity (2000–2006), with the predicted vertical displacement and change in gravity from GIA modelling. The geodetic results have mutual self-consistency, suggest station stability and provide upper bounds on both GIA and secular ice mass changes. The GIA models tend to predict amplitudes of rock motion larger than those observed, and we conclude that this part of Antarctica is probably experiencing a slight gain in ice mass, in contrast to West Antarctica.
Keywords: Absolute gravity, Antarctica, DORIS, Dumont d'Urville, GPS, tide gauge
Programme: 337
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Amalvict, M., R. Bayer, S. Bonvalot, N. Debeglia, M. Diament, F. Duquenne, H. Duquenne, J. Hinderer, M.-F. Lalancette, N., Le Moigne, B. Luck, G. Martelet, & M. Sarrailh. (2007). French activities in ground gravimetry Rapport quadriennal 2003-2007 du CNFGG.
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Amalvict, M., Rogister, Y , Luck B. & Hinderer J. (2007). Absolute gravity in the Southern Indian Ocean. IAG Symposia, 130, 433–437.
Abstract: in IAG Symposia 'Dynamic Planet: Monitoring and understanding a dynamic planet with geodetic and oceanographic tools
Programme: 337
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Amalvict, M., Rogister, Y., McQueen, H., Hinderer, J., & Luck, B. (2006). Absolute gravity experiments in Terre Adélie (Antarctica) and at Canberra & Tidbinbilla (Australia),.
Abstract: 1st Int. Gravity Field Service, Istanbul, Turkey.
Programme: 337
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