Petrotrama de quartzo e feldspato ao longo da Zona de Cisalhamento de Jundiuvira, Cabreuva (SP)

dc.contributorUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T11:17:55Z
dc.date.accessioned2022-10-05T17:28:52Z
dc.date.available2014-05-27T11:17:55Z
dc.date.available2022-10-05T17:28:52Z
dc.date.created2014-05-27T11:17:55Z
dc.date.issued1993-12-01
dc.identifierGeociencias (Sao Paulo), v. 12, n. 1, p. 141-153, 1993.
dc.identifierhttp://hdl.handle.net/11449/64428
dc.identifier2-s2.0-0027798520
dc.identifier1040135935908734
dc.identifier0000-0003-2125-3050
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3914485
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 summary
dc.languagepor
dc.relationGeociencias (Sao Paulo)
dc.rightsAcesso restrito
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)
dc.typeArtigo


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