The great escape: Petrogenesis of low-silica volcanism of Pliocene to Quaternary age associated with the Altiplano-Puna Volcanic Complex of northern Chile (21°10′-22°50′S)

@article{GonzlezMaurel2019TheGE,
  title={The great escape: Petrogenesis of low-silica volcanism of Pliocene to Quaternary age associated with the Altiplano-Puna Volcanic Complex of northern Chile (21°10′-22°50′S)},
  author={Osvaldo Gonz{\'a}lez-Maurel and Petrus J. le Roux and Benigno Godoy and Valentin R. Troll and Frances M Deegan and Andrew Menzies},
  journal={Lithos},
  year={2019}
}
10 Citations
Constraining the sub-arc, parental magma composition for the giant Altiplano-Puna Volcanic Complex, northern Chile
TLDR
New olivine and clinopyroxene oxygen isotope data from rare mafic volcanic rocks erupted at the margins of the giant Altiplano-Puna Magma Body (APMB) of the Altiplanos Volcanic Complex, Central Andes are presented, allowing us to estimate the δ 18 O values of sub-arc, parental melts to be estimated.
An Overview of the Mafic and Felsic Monogenetic Neogene to Quaternary Volcanism in the Central Andes, Northern Chile (18-28°Lat.S)
Monogenetic volcanism produces small eruptive volumes with short eruption history, different chemical compositions, and relatively simple conduit. The Central Volcanic Zone of the Andes is
Eruptive history of La Poruña scoria cone, Central Andes, Northern Chile
New stratigraphic, lithological and petrographic analyses of La Poruña scoria cone (21° 53′ S-68° 30′ W, Central Andes, northern Chile) allow the reconstruction of the eruptive sequence of this
Remote Sensing Survey of Altiplano-Puna Volcanic Complex Rocks and Minerals for Planetary Analog Use
The Altiplano-Puna Volcanic Complex (APVC) of the Central Andes is an arid region with extensive volcanism, possessing various geological features comparable to those of other solar system objects.

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