The detritic rocks of Ortaköy area were undergone a regional
metamorphism which caused development of the paragenesis: sillimanite +
plagioclase (An 0.43) +
orthoclase + quartz + biotite (Ann 0.08, Phl0.012) + garnet
(Alm 0.80-0.83, prP 0.10- 0.08 Sp 0.048-047 Grs 0.048-0.045).By geothermobarometers of garnet-biotite and
garnet-aliiminosilicate-quartz-plagioclase, the regional metamorphism
conditions were determined as P= 3.3±0,36 kb and T=~600°C. The garnet has
inverse mineralogical zoning due to homogenisation or exchange reaction between
garnet and matrix. Decreasing of grossulerite content in the garnet towards its
rim, and occurence of andalusite, chlorite and sericite show that P-T
conditions in Ortaköy area follows a clockwise path in P-T-t trajectory.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Mart 2000 |
Yayımlandığı Sayı | Yıl 2000 Cilt: 122 Sayı: 122 |
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