Transtension driving volcano-edifice anatomy: Insights from Andean transverse-to-the-orogen tectonic domains.

Quaternary International

dc.creatorSielfeld, G.
dc.creatorCembrano, J.
dc.creatorLara, L.
dc.date2020-03-11T20:27:07Z
dc.date2022-07-07T23:46:06Z
dc.date2020-03-11T20:27:07Z
dc.date2022-07-07T23:46:06Z
dc.date2016
dc.date.accessioned2023-08-22T02:24:57Z
dc.date.available2023-08-22T02:24:57Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238209
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8310420
dc.descriptionDykes and minor eruptive vents are not randomly distributed within tectonically controlled volcanic arcs, which is reflected in the resulting morphology of stratovolcanoes. As a first-order approach, regional stress field controls the spatial distribution
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.quaint.2016.01.002
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleTranstension driving volcano-edifice anatomy: Insights from Andean transverse-to-the-orogen tectonic domains.
dc.titleQuaternary International
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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