TY  - JOUR
TT  - Zey-1 Ve Zey-2 Kuyularındakî Karaboğaz Formasyonunun Organik Jeokîmyasal Açıdan 1ncelenmesî
AU  - Kavak, Orhan
PY  - 1999
DA  - June
Y2  - 1999
JF  - Eskişehir Osmangazi Üniversitesi Mühendislik ve Mimarlık Fakültesi Dergisi
JO  - ESOGÜ Müh Mim Fak Derg
PB  - Eskişehir Osmangazi Üniversitesi
WT  - DergiPark
SN  - 2630-5712
SP  - 58
EP  - 76
VL  - 12
IS  - 1
KW  - Organik Jeokimya. Kaynak Kaya. Pirola
KW  - GC
KW  - GC-MS.
N2  - Zey-1 ve 'iey-2 kmvlarmdaki Koraboğaz formasyonmun jeotimyasal özelliklerifalifilmifl:r Kuyulardaki Karabogaz formasyonundan almaıı örneklerden yapılan organikjeokimyasal analizler yardımıyla birimin kaynak kaya potaılsiyeline yönelik parametreler redeğişimleri saplanmıştır. Bu amaçla 3 adet Toplam organik karbon, 3 adet f'iroliz, herkuyudan l' er Ozvtleme, ince kolon kromatografisi. Kolon kromatagrafisi. Gaz h-omalogra/lsianalizleri ve Zey-I kuyıısmdan I adet Gaz h-omatograjîsi-Külte spektrometresi analizisomıcumla Tuplam Organik Karbon (TOK) degerlermin 1. 18-1. 75 arasinda, Tmca. 'm 437-441V. Hl 166-1011 mgHC/gCorg arasinda değiştiği ve birimin genel oiarat TİP Ildenize! organikmadde içerdiği ve olgun olduğu tespit edilmiştir. Orgmrik madde miktar:. organik madde tipi veolgunlaşma düzeyi cıçısmdm ayrıntılı olarak degerlendirllen Karatogaz formasyonunun İyi birkaynak kaya putansiyeîme sahip olduğu saptanmîşîır.ANAHTAR KELİMELER: Organik Jeokimya. Kaynak Kaya. Pirola, GC, GC-MS
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