Organic facies characteristics in the Paleocene shale of the northern part of the Tuz Golu Basin, Central Anatolia, Turkey
ENERGY SOURCES, cilt.23, sa.8, ss.727-737, 2001 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Tam Makale
- Cilt numarası: 23 Sayı: 8
- Basım Tarihi: 2001
- Doi Numarası: 10.1080/009083101316862480
- Dergi Adı: ENERGY SOURCES
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Sayfa Sayıları: ss.727-737
- Anahtar Kelimeler: Tuz Golu, Haymana-Polatli, Bala, Kirkkavak formation, Karapinaryaylasi formation, organic facies, EVOLUTION
- Ankara Üniversitesi Adresli: Evet
Özet
Paleocene sequence in the Tuz Golu Basin displays a range of lithofacies that vary greatly in thickness. The Paleocene units are made up of sandstone, conglomerate, shale, and limestone. Organic-rich intervals are present in the Paleocene of marine shale with 0.02-1.88 wt% organic carbon content. Pyrolysis yields (S-1 + S-2 = 80-10100 ppm) indicate that some intervals within the Paleocene shale have weak to good gas potential. It contains type III organic matter based upon Rock-Eval pyrolysis assay. Both organic petrographic and geochemical parameters place the Paleocene shale of the Tuz Golu Basin within the CD and D or C organic facies of Jones (1987). The lower sulphur content (< 0.08%) in the Paleocene units point to normal marine depositional conditions. Maturity is high in the lower Paleocene units where T-max values are above 465