Çine güneyi ( Akçaova ) pegmatitlerinin jeolojisi ve petrojenezi
Başlık çevirisi mevcut değil.
- Tez No: 38309
- Danışmanlar: PROF.DR. ERDİNÇ KİPMAN
- Tez Türü: Yüksek Lisans
- Konular: Jeoloji Mühendisliği, Maden Mühendisliği ve Madencilik, Geological Engineering, Mining Engineering and Mining
- Anahtar Kelimeler: Aydın-Çine-Akçaova Köyü, Feldispatlar, Jeolojik harita, Pegmatit, Stratigrafi, Aydın-Çine-Akçaova Village, Feldspars, Geological map, Pegmatite, Stratigraphy
- Yıl: 1995
- Dil: Türkçe
- Üniversite: İstanbul Üniversitesi
- Enstitü: Fen Bilimleri Enstitüsü
- Ana Bilim Dalı: Belirtilmemiş.
- Bilim Dalı: Belirtilmemiş.
- Sayfa Sayısı: Belirtilmemiş.
Özet
SUMMARY Geology and Petrogeneais of the Southern Cine (Akcaova) Pegmatites! This study involves that to general geological working of south of Akcaova < Aydın ). In* addition to that has been emerged feldspar investigation and its formation about this region. The research space involves about 20 km3 inside of Aydın N20-al section. It has been prepared geological maps about 1/25.000 and 1/5.000 scales of the region. Moreover it has been submitted to generalizing of stratigraphy scale. The rock units have been to named and selected on the map space by me. The oldest rock units of map scale are Ak caova metamorphies which is belong to paleozoic. It's reser- red hole-granitic gnays at the bottom of Akcaova metamorphies This unit is constituted the nucleus of Menderes massive, schists and quartsz which occur on the top of these massive. It's existed widely known feldspar occurances inside of gnays On the other hand, albitization is quite expanded in working area too. To hang on to metamorphies that this albitization expansion changes this area place to place. These industrial raw materials which find out from this area that are used frequently ceramic and usually glass industry. -98-The samples which has been collected -from working area and It has been explained its results -for text detaily. On the other hand, it has been worked the petrographic investi gations o-f the rocks which has been prepared tenuous sections On this occasion, It has been recognised the types o-f -feldspars. Anyway, It has been evaluated structruel elements sepa rately like -fault and articulation according to their relati ons with the helpness o-f collected i n-format ions in this area and it has been emerged the structural spec i -f i cat i ons to the area. -99-
Özet (Çeviri)
SUMMARY Geology and Petrogeneais of the Southern Cine (Akcaova) Pegmatites! This study involves that to general geological working of south of Akcaova < Aydın ). In* addition to that has been emerged feldspar investigation and its formation about this region. The research space involves about 20 km3 inside of Aydın N20-al section. It has been prepared geological maps about 1/25.000 and 1/5.000 scales of the region. Moreover it has been submitted to generalizing of stratigraphy scale. The rock units have been to named and selected on the map space by me. The oldest rock units of map scale are Ak caova metamorphies which is belong to paleozoic. It's reser- red hole-granitic gnays at the bottom of Akcaova metamorphies This unit is constituted the nucleus of Menderes massive, schists and quartsz which occur on the top of these massive. It's existed widely known feldspar occurances inside of gnays On the other hand, albitization is quite expanded in working area too. To hang on to metamorphies that this albitization expansion changes this area place to place. These industrial raw materials which find out from this area that are used frequently ceramic and usually glass industry. -98-The samples which has been collected -from working area and It has been explained its results -for text detaily. On the other hand, it has been worked the petrographic investi gations o-f the rocks which has been prepared tenuous sections On this occasion, It has been recognised the types o-f -feldspars. Anyway, It has been evaluated structruel elements sepa rately like -fault and articulation according to their relati ons with the helpness o-f collected i n-format ions in this area and it has been emerged the structural spec i -f i cat i ons to the area. -99-
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