
GEOTERMOBAROMETRIA EM ROCHAS DO COMPLEXO CAMPOS GERAIS AO NORTE DA ZONA DE CISALHAMENTO VARGINHA
1994; Sociedade Brasileira de Geologia; Linguagem: Inglês
10.25249/0375-7536.1994233239
ISSN2177-4382
AutoresELIANE APARECIDA DEL LAMA, Marcos Aurélio Farias de Oliveira, Antenor Zanardo,
Tópico(s)Geography and Environmental Studies
ResumoVARGINHA SHEAR ZONE.Electron microprobe chemical analysis of mineral species from rocks of the southern part of Campos Gerais Complex, São Pedro da União-Nova Resende region (MG) show that the analysed species have a relatively homogeneous composition and that their paragenesis and geothermometric calculations indicate that the peak metamorphism took place at temperatures of 830-900°C and pressures of 12.5-15.0kbar, the most common values being of 700-750°C and 11.8-12.1 kbar.The average geothermal gradient was of 21°C/km is obtained and is similar to that of the Araxá-Canastra Group.The general estimated metamorphic conditions are of high pressure, at least higher than the Barrowian type.
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