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The Bahram-Gur area in the southeastern part of the Sanandaj–Sirjan metamorphic zone, contains metabasites and metasediments. The metasedimentary rocks are mainly garnet schists and garnet-staurolite schists that were metamorphosed under amphibolite facies conditions. The rocks consist of garnet ± staurolite, biotite, muscovite, chlorite and quartz. The geochemistry of the Bahram-Gur metasediments classifies them as quartziferous sedimentary rocks. The protoliths of the metasedimentary rocks were close to greywackes from an ensialic arc basin depositional setting, with a source comprising mostly mixture of acid and intermediate magmatic rocks in the upper continental crust. The metamorphic conditions of formation of the Bahram-Gur metasedimentary are investigated by geothermobarometric methods. The results show that the metasedimentary rocks formed at temperatures of 600-750°C and pressures of 5-7.5 kbar.
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34--68
Opis fizyczny
Bibliogr. 65 poz., rys., tab., wykr.
Twórcy
autor
- Department of Geology, College of Sciences, Shahid Bahonar University, Kerman, 76176, Iran
autor
- Department of Geology, College of Sciences, Shahid Bahonar University, Kerman, 76176, Iran
autor
- Earth and Environmental Sciences Department, University Yamagata, Yamagata990, Japan
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-48e87871-9cb6-49fd-90b5-a0aba226e24d