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Identifying potentially active volcanoes in the Andes: Radiometric evidence for late Pleistocene-early Holocene eruptions at Volcán Imbabura, Ecuador
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“el Tayta (padre) Imbabura con 4620 metros sobre el nivel del mar (msnm) es el edificio principal, el Cubilche con 3826 msnm es el edificio más pequeño, el Artezón con 4137 msnm es un pico satelital y el Huarmi (mujer) Imbabura con 3926 msnm es el domo de lava con apariencia más joven (Le Pennec et al. 2011: 122).”
From Diversidad cultural en la utilización del paisaje: una interpretación geoarqueológica para la construcción de montículos artificiales entre los grupos karanki-kayampi de la sierra norte del ecuador (2020) · cites this paper as Le Pennec et al. 2011: 122
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Why Archaean TTG cannot be generated by MORB melting in subduction zones
Martin, H., Moyen, J.-F., Guitreau, M., Blichert-Toft, J., & Le Pennec, J.-L. (2014) · Lithos · doi:10.1016/j.lithos.2014.02.017 · Cited by 346
Self-citationLópez Soria, G., & Serrano Ayala, S. (2020) · Boletín de Arqueología PUCP · doi:10.18800/boletindearqueologiapucp.202001.001 · Cited by 1
Metadata
- Authors
- Le Pennec, J. L., Ruiz, A. G., Eissen, J. P., Hall, M. L., & Fornari, M.
- Venue
- Journal of Volcanology and Geothermal Research
- Publisher
- Elsevier BV
- Published
- 2011-09
- Volume
- 206
- Issue
- 3-4
- Pages
- 121-135
- ISSN
- 0377-0273
- Cited by
- 22
- References
- 0
- Language
- en
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