Magma evolution of Quaternary minor volcanic centres in southern Peru, Central Andes

@article{Delacour2007MagmaEO,
  title={Magma evolution of Quaternary minor volcanic centres in southern Peru, Central Andes},
  author={Adélie Delacour and Marie C. Gerbe and Jean-Claude Thouret and Gerhard W{\"o}rner and Perrine Paquereau-Lebti},
  journal={Bulletin of Volcanology},
  year={2007},
  volume={69},
  pages={581-608}
}
Minor centres in the Central Volcanic Zone (CVZ) of the Andes occur in different places and are essential indicators of magmatic processes leading to formation of composite volcano. The Andahua–Orcopampa and Huambo monogenetic fields are located in a unique tectonic setting, in and along the margins of a deep valley. This valley, oblique to the NW–SE-trend of the CVZ, is located between two composite volcanoes (Nevado Coropuna to the east and Nevado Sabancaya to the west). Structural analysis… 
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