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dc.contributor.authorSen, Samil
dc.date.accessioned2021-03-04T17:39:37Z
dc.date.available2021-03-04T17:39:37Z
dc.date.issued2017
dc.identifier.citationSen S., "Unconventional oil and gas system of the Upper Jurassic Akkuyu formation in the Tauride belt, Eastern Mediterranean", PETROLEUM SCIENCE AND TECHNOLOGY, cilt.35, sa.9, ss.896-902, 2017
dc.identifier.issn1091-6466
dc.identifier.othervv_1032021
dc.identifier.otherav_869d40ed-ca46-499f-9a1a-f9ec403380c9
dc.identifier.urihttp://hdl.handle.net/20.500.12627/91487
dc.identifier.urihttps://doi.org/10.1080/10916466.2017.1302473
dc.description.abstractThe Upper Jurassic Akkuyu formation of the Akseki platform is comprised of a 200m thick unit of organic rich carbonate mudstones. TOC contents range from 0.62 to 19.42% and %Rocal values are between 0.51 and 2.85. Thus, carbonate mudstones of the Akkuyu formation have excellent potential to early-middle mature oil and dry gas. Corrected oil saturation indexes of the mudstones show that the formation has no potentially producible oil possibly due to their hybrid and fractured oil. XRD whole rock analyses suggest that these carbonate mudstones are comprised of 85-100% calcite and dolomite, 0-5% quartz, and 0-10% clay.
dc.language.isoeng
dc.subjectTarımsal Bilimler
dc.subjectENERJİ VE YAKITLAR
dc.subjectMühendislik
dc.subjectMühendislik, Bilişim ve Teknoloji (ENG)
dc.subjectMÜHENDİSLİK, KİMYASAL
dc.subjectMÜHENDİSLİK, PETROL
dc.subjectZiraat
dc.subjectTarım Makineleri
dc.subjectTarımda Enerji
dc.subjectBiyoyakıt Teknolojisi
dc.subjectKimya Mühendisliği ve Teknolojisi
dc.subjectPetrol ve Doğal Gaz Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.titleUnconventional oil and gas system of the Upper Jurassic Akkuyu formation in the Tauride belt, Eastern Mediterranean
dc.typeMakale
dc.relation.journalPETROLEUM SCIENCE AND TECHNOLOGY
dc.contributor.departmentİstanbul Üniversitesi , Mühendislik , Jeoloji
dc.identifier.volume35
dc.identifier.issue9
dc.identifier.startpage896
dc.identifier.endpage902
dc.contributor.firstauthorID238690


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