Organic Geochemical Properties of Marine Oligocene Unit in the Malatya Basin, East Anatolia, Turkey

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Atıf İçin Kopyala

Onal M.

ENERGY SOURCES PART A-RECOVERY UTILIZATION AND ENVIRONMENTAL EFFECTS, cilt.31, sa.15, ss.1406-1414, 2009 (SCI-Expanded)

• Yayın Türü: Makale / Tam Makale
• Cilt numarası: 31 Sayı: 15
• Basım Tarihi: 2009
• Doi Numarası: 10.1080/15567030802092726
• Dergi Adı: ENERGY SOURCES PART A-RECOVERY UTILIZATION AND ENVIRONMENTAL EFFECTS
• Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
• Sayfa Sayıları: ss.1406-1414
• İnönü Üniversitesi Adresli: Hayır

Özet

Organic geochemical properties of the Oligocene unit in the Malatya Basin: Darende-Hekimhan section's TOC and genetic potential values range from 0.06 to 13.94 wt% and 110 to 94,490 ppm. Low total organic carbon (TOC) and genetic potential (GP) values indicate that the Oligocene unit has no source rock potential, except Darende-Hekimhan section. Organic matter type of the sequences is type II, indicating marine origin; however, Darende-Hekimhan section samples show that Type I, indicate lacustrine origin from HI-OI diagram, having low T-max values (between 345 degrees C and 419 degrees C). Oligocene sequences are able to have mature source rock potential in the deeper part of the basin.