Organic geochemical properties of marine Oligocene unit in the Malatya basin, east Anatolia, Turkey
Yazarlar (1)
Prof. Dr. Mehmet Mustafa ÖNAL Kırşehir Ahi Evran Üniversitesi, Türkiye
Makale Türü Özgün Makale (Uluslararası alan indekslerindeki dergilerde yayınlanan tam makale)
Dergi Adı Energy Sources, Part A
Makale Dili Basım Tarihi 08-2009
Cilt / Sayı / Sayfa 31 / 15 / 1406–1414 DOI 10.1080/15567030802092726
Makale Linki https://www.tandfonline.com/doi/abs/10.1080/15567030802092726
UAK Araştırma Alanları
Betonarme Yapılar
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 Tmax values (between 345°C and 419°C). Oligocene sequences are able to have mature source rock potential in the deeper part of the basin.
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Organic geochemical properties of marine Oligocene unit in the Malatya basin, east Anatolia, Turkey

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