Pondrelli S., L. Margheriti and S. Danesi. (2005). Seismic anisotropy beneath Northern Victoria Land from SKS splitting analysis, Antarctica. Bachelor's thesis, Springer-Verlag Berlin Heidelberg Eds, .
Abstract: Contr.
to Global Earth Sciences, Springer-Verlag Berlin Heidelberg Eds.
Programme: 906
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Marino F., G. Calzolai, S. Caporali, E. Castellano, M. Chiari, F. Lucarelli, V. Maggi, S. Nava, M. Sala, R. Udisti. (2008). PIXE and PIGE techniques for the analysis of Antarctic ice dust and continental sediments. Nuclear instruments and methods in physics research b, 266, 2396–2400.
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Cagnati A., Dicasillati R., Salvietti E. & Udisti R. (2008). Snow crystal observations at Dome C, Antarctica. Terra antarctica, 14, 147–150.
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Marino F., S. Becagli, E. Castellano, A Mannini, E. Salvietti, O. Cerri, R. Traversi, S. Caporali, V. Maggi, R. Udisti. (2008). Geochemical characterization of present-day dust by all-year-round high-volume aerosol sampling: planned activity for the 2005-2006 Dome C campaign. Terra antarctica, 14, 89–96.
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Udisti R., S. Becagli, E. Castellano, O. Cerri, A. Mannini, F. Marino, A. Morganti, E. Salvietti, M. Severi, R. Traversi. (2008). 2004-05 summer and winter-over campaign for aerosol sampling at dome c (east Antarctica): sampling strategies and first results. Terra antarctica, 14, 187–198.
Abstract: Terra Antarctica Report, 2008, 14, 187-198.
Programme: 1181
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Becagli S., E. Castellano, O.Cerri, M. Chiari, F. Lucarelli, F. Marino, A. Morganti, S. Nava, F. Rugi, M. Severi, R. Traversi, V. Vitale, R. Udisti. (2008). All year round background aerosol at Dome C (Antarctica). Chemical composition of size-segregated samples collected during the 2004-05 campaign. Bachelor's thesis, , .
Abstract: 2008, SIF – Bologna, in press.
Programme: 1181
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Macelloni G., Brogioni M., Pampaloni P. , Drinkwater M., Cagnati A. (2006). DOMEX 2004: an Experimental Campaign at Dome-C Antarctica for the Calibration of Space-Borne Low-Frequency Microwave Radiometers. Transactions of geoscience and remote sensing, 44(10), 2642–2653.
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Macelloni G.,Brogioni M.,Pampaloni P., Cagnati A. (2007). Multi-frequency Microwave Emission from the East Antarctic Plateau:Temporal and Spatial Variability. Transactions of geoscience and remote sensing, 45(7 part1).
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Cagnati A. , Macelloni G. , Salvietti E. & M. Valt. (2008). Snow Surface Characteristics at Dome C, Antarctica. Terra antarctica, 14, 151–154.
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Geoffroy, L.; Aubourg, C.; Callot, J.-P.; Barrat, J.-A. (2007). Mechanisms of crustal growth in large igneous provinces: The north Atlantic province as a case study. Geological Society of America Special Papers, 430, 747–774.
Abstract: The mechanisms of magma crust accretion at large igneous provinces (LIPs) are questioned using arguments based on the north Atlantic case. Published and new data on the calculated flow vectors within dike swarms feeding the early traps and subsequent seaward-dipping reflector lavas suggest that most of the mafic magmas forming the north Atlantic LIP transited through a small number of igneous centers. The magma was injected centrifugally in dike swarms at some distance away from individual igneous centers along the trend of the maximum horizontal stress acting in the crust, feeding lava piles via dikes intersecting the ground surface. This mechanism is similar to that observed in present-day Iceland and, more generally, in mafic volcano-tectonic systems. The absence of generalized vertical magma transit in a LIP has major geodynamic consequences. We cannot link the surface extent of LIP magmas to the dimensions of the mantle melting zone as proposed in former plume head models. The distribution of LIP magmas at the surface is primarily controlled by the regional stress field acting within the upper crust, but is also affected by magma viscosity. The igneous centers feeding LIPs most likely represent the crustal expression of small-scale convective cells of the buoyant mantle naturally located beneath the mechanical lithosphere.
Keywords: traps; volcanic margin; dike swarm; small-scale convection; AMS
Programme: 290
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