Stratigraphy, geochronology and evolution of the Mt. Melbourne volcanic field (North Victoria Land, Antarctica)

@article{Giordano2012StratigraphyGA,
  title={Stratigraphy, geochronology and evolution of the Mt. Melbourne volcanic field (North Victoria Land, Antarctica)},
  author={Guido Giordano and Federico Rodr{\'i}guez Lucci and David Phillips and Domenico Cozzupoli and Valentina Runci},
  journal={Bulletin of Volcanology},
  year={2012},
  volume={74},
  pages={1985-2005}
}
Mt. Melbourne (2,732 m a.s.l.) is a large quiescent stratovolcano located in Northern Victoria Land (Antarctica) and is one of a handful of volcanoes on the Antarctic plate with the potential for large-scale explosive eruptions. During the XVIII Italian Expedition in 2002–2003, the Mt. Melbourne volcanic succession was studied in terms of stratigraphy and sampled for 40Ar/39Ar age determinations and geochemistry. The early, Lower Pleistocene, volcanism was largely alkali basaltic to hawaiitic… 
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