Ultramafic rocks in the north patagonian andes: Is their emplacement associated with the neogene tectonics of the liquiñe-ofqui fault zone?

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dc.contributor.authorHervé, Francisco
dc.contributor.authorFuentes, Francisco
dc.contributor.authorCalderón, Mauricio
dc.contributor.authorFanning, Mark
dc.contributor.authorQuezada, Paulo
dc.contributor.authorPankhurst, Robert
dc.contributor.authorRapela, Carlos
dc.date.accessioned2024-09-17T16:37:02Z
dc.date.available2024-09-17T16:37:02Z
dc.date.issued2017-01
dc.descriptionIndexación: Scopus
dc.description.abstractSerpentinites and fresh or partially serpentinized harzburgite crop out in the western slope of the North Patagonian Andes of continental Chiloé (41°44’-42°12’S). These rocks are spatially associated with low-grade metamorphic rocks containing Cenozoic detrital zircons. The metamorphic rocks, together with Devonian metasediments, have been mapped previously as Late Paleozoic-Triassic metamorfic complex, an age no longer tenable for at least part of the complex. Transpressional tectonic emplacement of the ultramafic body or bodies is thought to have been related to activity on the Liquiñe-Ofqui Fault Zone, following a late Oligocene-Early Miocene extensional phase in the forearc region of the present Andes. This fault zone occurs immediately east of the outcrops of the ultramafic rocks and has been interpreted previously as generating a hemi-flower or flower structure. © 2017, Servicio Nacional de Geologia y Mineria. All Rights Reserved.
dc.description.urihttp://www.andeangeology.cl/index.php/revista1/article/view/V44n1-a01
dc.identifier.citationAndean Geology Volume 44, Issue 1, Pages 1 - 16January 2017
dc.identifier.doi10.5027/andgeoV44n1-a01
dc.identifier.issn0718-7092
dc.identifier.urihttps://repositorio.unab.cl/handle/ria/60265
dc.language.isoes
dc.publisherServicio Nacional de Geologia y Mineria
dc.rights.licenseAttribution 4.0 International CC BY 4.0 Deed
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectLiquiñe-Ofqui fault zone
dc.subjectNeogene tectonics
dc.subjectNorth patagonian andes
dc.subjectSerpentinites
dc.titleUltramafic rocks in the north patagonian andes: Is their emplacement associated with the neogene tectonics of the liquiñe-ofqui fault zone?
dc.title.alternative[Rocas ultramáficas en los Andes norpatagónicos: ¿está su emplazamiento asociado a la actividad tectónica Neógena de la Zona de Falla Liquiñe-Ofqui?]
dc.typeArtículo
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