Arizaro volcanic field is a group of volcanoes west of the Salar de Arizaro.
| Arizaro volcanic field | |
|---|---|
  Arizaro volcanic field | |
| Highest point | |
| Coordinates | 24°45′00″S 68°02′30″W / 24.75000°S 68.04167°W[1] |
The volcanic field lies above the western shores of the Salar de Arizaro. It consists of numerous Pleistocene basaltic andesite lava flows, as well as cinder cones with Holocene basaltic lava flows. Most centres are roughly aligned in northeast-southwest direction.[1] The Arizaro volcanic field is part of a wider area of mafic volcanism in the Puna[2] that includes Holocene activity.[3] It is considered the second-least dangerous volcano in Argentina.[4]
The volcanic field lies in the Puna, a high plateau generated by the subduction of the Nazca Plate beneath the South America Plate.[5] The terrain consists mainly of Miocene volcaniclastic rocks with a single outcrop of Ordovician granodiorite. Parts of the area are covered by Quaternary alluvium and conglomerates. The basement rocks are influenced by normal faulting.[1]
The volcanism in the field has been explained by lithospheric delamination, a process by which part of the lower lithosphere founders into the mantle. Such a process is accompanied by uplift of the abovelying crust and often by volcanism of mainly small volume. Seismic imagery has been used to argue for the existence of delaminated crust in the mantle above the downgoing Nazca Plate slab beneath the Arizaro region.[5]
The age of the lavas has been determined by argon-argon dating. The northernmost lava flow has yielded an age of 80,000 ± 60,000 years before present, while a southern lava flow has been dated to 130,000 ± 10,000 years before present and a date of 2.52 ± 0.05 million years ago was found on a central lava flow;[6] this last lava flow shows evidence of younger faulting.[7]
References
edit- ^ a b c Schoenbohm & Carrapa 2015, p. 170.
- ^ Grosse et al. 2020, p. 2.
- ^ Viramonte et al. 1984, p. 234.
- ^ Garcia & Badi 2021, p. 26.
- ^ a b Schoenbohm & Carrapa 2015, p. 168.
- ^ Schoenbohm & Carrapa 2015, p. 170,173.
- ^ Schoenbohm & Carrapa 2015, p. 173.
Sources
edit- Garcia, Sebastian; Badi, Gabriela (1 November 2021). "Towards the development of the first permanent volcano observatory in Argentina". Volcanica. 4 (S1): 21–48. doi:10.30909/vol.04.S1.2148. ISSN 2610-3540.
- Grosse, Pablo; Ochi Ramacciotti, María Luisa; Escalante Fochi, Florencia; Guzmán, Silvina; Orihashi, Yuji; Sumino, Hirochika (September 2020). "Geomorphology, morphometry, spatial distribution and ages of mafic monogenetic volcanoes of the Peinado and Incahuasi fields, southernmost Central Volcanic Zone of the Andes". Journal of Volcanology and Geothermal Research. 401: 106966. doi:10.1016/j.jvolgeores.2020.106966.
- Schoenbohm, Lindsay M.; Carrapa, Barbara (2015). "Miocene–Pliocene shortening, extension, and mafic magmatism support small-scale lithospheric foundering in the central Andes, NW Argentina". Geodynamics of a Cordilleran Orogenic System: The Central Andes of Argentina and Northern Chile. pp. 167–180. doi:10.1130/2015.1212(09). ISBN 9780813712123.
- Viramonte, J. G.; Galliski, M. A.; Araña Saavedra, V.; Aparicio, A.; García Cacho, L.; Martín Escorza, C. (1984). El finivulcanismo básico de la depresión de Arizaro, provincia de Salta. 9th Argentine Geological Congress. pp. 234–251 – via ResearchGate.