Microseismic reflection imaging of the Central Andean crust

dc.date.accessioned2020-03-11T20:29:26Z
dc.date.accessioned2022-10-18T22:46:53Z
dc.date.available2020-03-11T20:29:26Z
dc.date.available2022-10-18T22:46:53Z
dc.date.created2020-03-11T20:29:26Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/238811
dc.identifier15110017
dc.identifierWOS:000368427100052
dc.identifierno scielo
dc.identifiereid=2-s2.0-84958617001
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4470150
dc.description.abstractThe coda of passive seismic recordings is often rich in arrivals that are coherent across several stations. If reflections can be extracted, then they may be used for seismic reflection subsurface imaging. With the objective to image the upper crust of th
dc.languageeng
dc.relationhttps://doi.org/10.1093/gji/ggv530
dc.relation10.1093/gji/ggv530
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.titleMicroseismic reflection imaging of the Central Andean crust
dc.typeArticulo


Este ítem pertenece a la siguiente institución