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    Geological map of southern Argentera Massif (Maritime Alps)
    Roberto Malaroda
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    Characters and genetic significance of the pseudoporphyric gneisses in the Argentera Massif (Maritime Alps)
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    3D geological modeling as a tool for geothermal prospection in the argentera massif (South-western Alps)
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    Geoelectrical soundings in the Combeynot Massif (French Alps) : Characterisation of Alpine permafrost and geodynamics of the Southern Alps .
    HAL (Le Centre pour la Communication Scientifique Directe) (2007)
    Xavier BodinDenis FabreAdriano RiboliniPhilippe SchoeneichMonique Fort
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    Geoelectrical soundings in the Combeynot Massif (French Alps): characterisation of alpine permafrost in the Southern Alps
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    The rock glaciers of Argentera Crystalline Massif, Italian side, Maritime Alps
    Adriano Ribolini
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    Stratigraphic and tectonic setting of the southern termination of the Western Alps (Ligurian-Maritime Alps junction): an update
    Luca BaraleCarlo BertokAnna Raffaella D'AtriLuca MartireFabrizio Piana
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    Geological map of the San Donato – Costa Thrust Zone, Belluno Thrust System, eastern Southern Alps (northern Italy)
    Journal of Maps (2021)
    Costantino ZuccariGianluca VignaroliGiulio Viola
    We present a 1:7500 scale geological map of part of the footwall of the south verging Belluno Thrust of the seismically active eastern Southern Alps of northern Italy. We report a previously unknown thrust zone, the "San Donato-Costa Thrust Zone", that cuts across the local Meso-Cenozoic stratigraphic succession. 1:2500 and 1:5000 geological mapping, in combination with the revision and improvement of the local lithostratigraphy and detailed structural analysis, provided new insights into the thrust geometry and the setting of the greater area it deforms. We show that the recorded deformation style (e.g. folding vs. faulting) exhibits notable variations within the affected Meso-Cenozoic stratigraphic succession, with shortening accommodated by fold trains and several subparallel thrust splays with variable amounts of stratigraphic offset cumulated during repeated faulting. Our results contribute to a better definition of folding and faulting within the Mesozoic carbonate multilayer system of the eastern Southern Alps.
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    Lithostratigraphy
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    Surface ground temperatures of rock glaciers in the Argentera Massif (Maritime Alps, Italy): one year of monitoring.
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    Massif
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