dc.creatorSielfeld, Gerd
dc.creatorCembrano-Perasso, José Miguel
dc.creatorLara, Luis
dc.date2019-03-27T15:56:50Z
dc.date2022-06-18T19:34:55Z
dc.date2019-03-27T15:56:50Z
dc.date2022-06-18T19:34:55Z
dc.date2014
dc.date2014
dc.date2014
dc.date.accessioned2023-08-22T08:56:58Z
dc.date.available2023-08-22T08:56:58Z
dc.identifier1141139
dc.identifierhttps://hdl.handle.net/10533/233623
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8334824
dc.descriptionLong and short-­‐term tectonic activity plays an essential role in the segregation, transport and emplacement of fluids and magmas within the continental crust. Magma ascent and emplacement mechanisms within volcanic arcs are largely controlled by the int
dc.descriptionFONDECYT
dc.descriptionFONDECYT
dc.languageeng
dc.relationAGU (American Geophysical Union) Fall Meeting
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1141139
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleTranstension controlling volcanic morphology: Insights from oblique-to-the arc tectonic domains
dc.typePonencia
dc.coverageSan Francisco


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