dc.creatorAciar, Rafael Hernán
dc.creatorLarrovere, Mariano Alexis
dc.creatorAgüero, Roberto Ariel
dc.date.accessioned2022-07-28T17:45:20Z
dc.date.accessioned2022-10-15T05:16:07Z
dc.date.available2022-07-28T17:45:20Z
dc.date.available2022-10-15T05:16:07Z
dc.date.created2022-07-28T17:45:20Z
dc.date.issued2019
dc.identifierAnálisis petrológico y estructural del basamento ígneo-metamórfico en la quebrada de Agua Negra, Cordillera de San Buenaventura, Catamarca; XIII Congreso de Mineralogía, Petrología Ígnea y Metamórfica, y Metalogénesis (XIII MINMET y IV PIMMA); Córdoba; Argentina; 2019; 214-215
dc.identifier978-987-86-1704-6
dc.identifierhttp://hdl.handle.net/11336/163436
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4348724
dc.description.abstractThe Cordillera de San Buenaventura forms a mountain range that extends from E-O to ESE-ONO and is located on the border between the Puna Austral and the Sierras Pampeanas. We analyze the petrology and the structure of the crystalline basement outcropping in the Agua Negra creek, located in the southern sector of the San Buenaventura range. This study determined that the area is constituted by mylonites, ultramilonites and granitoids without deforming. The deformation that affects the crystalline basement defines a ductile shear zone. The samples analyzed in thin section shows an intense recrystallization suggesting that the thermal conditions during the deformation were superior to 500 °C.
dc.languagespa
dc.publisherDahlquist, Juan Andrés
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://minmet-pimma-2019.congresos.unc.edu.ar/
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceCongreso de Mineralogía, Petrología Ígnea y Metamórfica, y Metalogénesis: XIII MINMET y IV PIMMA: actas
dc.subjectROCAS PLUTÓNICAS
dc.subjectMILONITAS
dc.subjectFAJA DE CIZALLA DÚCTIL
dc.subjectCORDILLERA DE SAN BUENAVENTURA
dc.titleAnálisis petrológico y estructural del basamento ígneo-metamórfico en la quebrada de Agua Negra, Cordillera de San Buenaventura, Catamarca
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeinfo:eu-repo/semantics/conferenceObject
dc.typeinfo:ar-repo/semantics/documento de conferencia


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