Isparta güneyinin jeolojisi ve maden yatakları
Başlık çevirisi mevcut değil.
- Tez No: 22206
- Danışmanlar: PROF. DR. ATASEVER GEDİKOĞLU
- Tez Türü: Yüksek Lisans
- Konular: Jeoloji Mühendisliği, Geological Engineering
- Anahtar Kelimeler: Ekonomik jeoloji, Isparta, Jeoloji, Maden yatakları, Stratigrafi, Economic geology, Isparta, Geology, Ore deposits, Stratigraphy
- Yıl: 1992
- Dil: Türkçe
- Üniversite: Akdeniz Üniversitesi
- Enstitü: Fen Bilimleri Enstitüsü
- Ana Bilim Dalı: Jeoloji Ana Bilim Dalı
- Bilim Dalı: Belirtilmemiş.
- Sayfa Sayısı: Belirtilmemiş.
Özet
ABSTRACT The studied Area, of about 200 km2, is located between Ağlasun District (Burdur) and the south of İsparta. The sequences, determined in the area, have been distinguished in two main groups, as autochthonous and allochthonous. The autochthonous have been ranged in age from Triassic Ispartaçay formation, the basement, to Pliocene Gölcük volcanics, actual aluvium and uncemented materials. The Cretaceous Davras formation, Eocene Savkoy formation, Lower Miocene Imrezi formation and Ağlasun formation and Upper Miocene Gavurdüzü formation were the other rocks observed in the area. The Al lochthonous sequences, defined in the area., were ophiolites and Akdaâj limestones. The single economics material in the area is the trass which have been used for years in Göltas Cement plant in İsparta as a raw material. The chemical properties of the trass as follows. The contents of SiOa+AlaAs+Fea-Os is 74-847.; of MgO 0.27-0.767. and of S0a 0.00-0.307.. These properties are very suitable for industrial marketing and as a result of geological, geochemical and other properties it has been conceded that the material can be used productively for cement industry as raw material.
Özet (Çeviri)
ABSTRACT The studied area, of about 20O km2, is located betveen Ağlasun District (Burdur) and the south of İsparta. The sequences, determined in the area, have been distinguished in two main groups, as autochthonous and allochthonous. The autochthonous have been ranged in age from Triassic Ispartacay formation, the basement, to Pliocene Gölcük volcanics, actual aluvium and uncemented materials. The Cretaceous Davras formation, Eocene Savköy formation, Lower Miocene Imrezi formation and Ağlasun formation and Upper Miocene Gavurdüzü formation were the other rocks observed in the area. The Allochthonous sequences, defined in the area, were ophiolites an'd Akdaâj limestones. The single economics material in the area is the trass which have been used for years in Göltas Cement plant in İsparta as a raw material. The chemical properties of the trass as follows. The contents of SiOa+AlaOa+FeîsOa is 74-847.; of MgO O.27-O.7S'/. and of 30=, O.OO-O.30'/.. These properties are very suitable for industrial marketing and as a result of geological, geochemical and other properties it has been conceded that the material can be used productively for cement industry as raw mater i al.
Benzer Tezler
- Isparta güneyi Ağlasun-Bucak dolayının jeolojik ve tektonik özellikleri
The geological and techtonical features around of Ağlasun-Bucak, southern of Isparta
METE HANÇER
Doktora
Türkçe
1996
Jeoloji MühendisliğiSüleyman Demirel ÜniversitesiJeoloji Mühendisliği Ana Bilim Dalı
PROF. DR. ERKAN KARAMAN
- Eğirdir-Burdur Gölleri arasının hidrojeolojik incelenmesi
Hydrogeology investigation of beween Eğirdir Lake-Burdur Lake
AYŞEN IRLAYICI
Doktora
Türkçe
1998
Jeoloji MühendisliğiSüleyman Demirel ÜniversitesiJeoloji Mühendisliği Ana Bilim Dalı
DOÇ. DR. REMZİ KARAGÜZEL
- Antalya traverten platosunun jeolojik, hidrolojik hidrojeolojik ve hidrokimyasal özelliklerinin incelenmesi
Başlık çevirisi yok
ALİ SERDAR ÖZÜŞ
Doktora
Türkçe
1992
Jeoloji MühendisliğiÇukurova ÜniversitesiJeoloji Mühendisliği Ana Bilim Dalı
PROF. DR. AZİZ ERTUNÇ
PROF. DR. SERVET YAMAN
- Isparta-Antalya arasında yer alan Anadolu Selçuklu Dönemi hanlarından“İncir Han”
“Incir Han”one of the Anatolian-Seljuks Period hans existing beetween Isparta-Antalya
ABDULLAH ŞEVKİ DUYMAZ
Yüksek Lisans
Türkçe
1996
Sanat TarihiHacettepe ÜniversitesiArkeoloji ve Sanat Tarihi Ana Bilim Dalı
PROF.DR. BEYHAN KARAMAĞARALI