Chusmiza

Chusmiza complex (also known as Cerros de Sotoca)[1] is a Miocene volcano in Chile. It is the largest stratovolcano of the Miocene in the western Andean escarpment, with a volume 400 cubic kilometres (96 cu mi). It is constructed from andesite.[2] Potassium-argon dating has established an age of 11.3±0.3 mya.[1]

References

  1. 1 2 Farías, Marcelo; Charrier, Reynaldo; Comte, Diana; Martinod, Joseph; Hérail, Gérard (August 2005). "Late Cenozoic deformation and uplift of the western flank of the Altiplano: Evidence from the depositional, tectonic, and geomorphologic evolution and shallow seismic activity (northern Chile at 19°30′S)". Tectonics. 24 (4). doi:10.1029/2004TC001667. Retrieved 1 October 2015.
  2. ↑ Wörner, Gerhard; Hammerschmidt, Konrad; Henjes-Kunst, Friedhelm; Lezaun, Judith; Wilke, Hans (December 2000). "Geochronology (40Ar/39Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from Northern Chile (18-22°S): implications for magmatism and tectonic evolution of the central Andes". Revista Geológica de Chile. Santiago: SciELO. 27 (2). doi:10.4067/S0716-02082000000200004. ISSN 0716-0208. Retrieved 1 October 2015.
This article is issued from Wikipedia - version of the 12/1/2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.