Petrotrama de quartzo e feldspato ao longo da Zona de Cisalhamento de Jundiuvira, Cabreuva (SP)
| Contribuinte(s) |
Universidade Estadual Paulista (UNESP) |
|---|---|
| Data(s) |
27/05/2014
27/05/2014
01/12/1993
|
| Resumo |
Fluid 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 |
| Formato |
141-153 |
| Identificador |
Geociencias (Sao Paulo), v. 12, n. 1, p. 141-153, 1993. http://hdl.handle.net/11449/64428 2-s2.0-0027798520 |
| Idioma(s) |
por |
| Relação |
Geociencias (Sao Paulo) |
| Direitos |
closedAccess |
| Palavras-Chave | #cataclasite #fabric #feldspar #fluid inclusion #mylonite #quartz #shear zone #Brazil, Sao Paulo |
| Tipo |
info:eu-repo/semantics/article |
