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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/64428
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dc.contributor.authorHackspacher, P. C.-
dc.contributor.authorGodoy, M. L S-
dc.contributor.authorSanto, E. L.-
dc.date.accessioned2014-05-27T11:17:55Z-
dc.date.accessioned2016-10-25T18:13:14Z-
dc.date.available2014-05-27T11:17:55Z-
dc.date.available2016-10-25T18:13:14Z-
dc.date.issued1993-12-01-
dc.identifier.citationGeociencias (Sao Paulo), v. 12, n. 1, p. 141-153, 1993.-
dc.identifier.urihttp://hdl.handle.net/11449/64428-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/64428-
dc.description.abstractFluid inclusions, petrofabric and microstructures studies of mylonites and cataclasites were used to establish the Itu-Jundiuvira Shear Zone (IJSZ) tectonic and metamorphic evolution. The quartz fabric indicates that prism {1000} slip was important during the deformation. This studies have showed that IJSZ changed from deeper crustal levels (12-15km) and ductile conditions to upper levels of about 4 to 6km and brittle strain conditions. -English summaryen
dc.format.extent141-153-
dc.language.isopor-
dc.sourceScopus-
dc.subjectcataclasite-
dc.subjectfabric-
dc.subjectfeldspar-
dc.subjectfluid inclusion-
dc.subjectmylonite-
dc.subjectquartz-
dc.subjectshear zone-
dc.subjectBrazil, Sao Paulo-
dc.titlePetrotrama de quartzo e feldspato ao longo da Zona de Cisalhamento de Jundiuvira, Cabreuva (SP)pt
dc.title.alternativeFeldspar and quartz petrofabric in the Jundiuvira Shear Zone, Cabreuva, SPen
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofGeociencias (Sao Paulo)-
dc.identifier.scopus2-s2.0-0027798520-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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