Geomorphology and structural development of the nested summit crater of Lascar Volcano studied with Terrestrial Laser Scanner data and analogue modelling

dc.date.accessioned2020-03-11T20:29:28Z
dc.date.accessioned2022-10-18T22:47:00Z
dc.date.available2020-03-11T20:29:28Z
dc.date.available2022-10-18T22:47:00Z
dc.date.created2020-03-11T20:29:28Z
dc.date.issued2017
dc.identifierhttp://hdl.handle.net/10533/238827
dc.identifier15110017
dc.identifierWOS:000392553700001
dc.identifierno scielo
dc.identifiereid=2-s2.0-85007316005
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4470166
dc.description.abstractMany volcano summits host craters that are partially overlapping. The formation of such nested craters has been commonly interpreted as vent migration. Here, we present an additional mechanism that may explain the geometry of nested craters at volcanoes.
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.jvolgeores.2016.09.018
dc.relation10.1016/j.jvolgeores.2016.09.018
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.titleGeomorphology and structural development of the nested summit crater of Lascar Volcano studied with Terrestrial Laser Scanner data and analogue modelling
dc.typeArticulo


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