has been cited by the following article(s):
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[1]
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Geochemistry and Reservoir Properties of the Upper Jurassic Formations, in Selected Oilfield Central Iraq
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IOP Conference Series: Earth and …,
2024 |
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[2]
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Dolomitization of the Lower Part of the Sargelu Formation, Northeastern Iraq
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Tikrit Journal of Pure Science,
2024 |
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[3]
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Integration of petrophysical and geochemical approaches for lower Miocene Euphrates and Jeribe Formations in selected wells in Tawke Oil Field, Northwestern Iraq …
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Journal of African Earth …,
2023 |
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[4]
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Determining of Dolomitization Age and Depth of Mardin Group Based on Clumped Isotopes and 1D Basin Model in SE Anatolia (SE Turkey) Güneydoğu Anadolu …
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Yerbilimleri/Earth …,
2022 |
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[5]
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Stratigraphic correlation and source rock characteristics of the Baluti formation from selected wells in the Zagros fold belt, Kurdistan Region, northern Iraq
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Journal of Petroleum …,
2022 |
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[6]
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Güneydo?u Anadolu B?lgesi Mardin Grubu dolomitlerinin dolomitle?me ya?lar?n?n ve derinliklerinin kümelenmi? izotoplar ve 1B basen modeli kullan?larak belirlenmesi
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Bulletin For Earth Sciences,
2022 |
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[1]
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Geochemistry and Reservoir Properties of the Upper Jurassic Formations, in Selected Oilfield Central Iraq
IOP Conference Series: Earth and Environmental Science,
2024
DOI:10.1088/1755-1315/1300/1/012031
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[2]
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Integration of petrophysical and geochemical approaches for lower Miocene Euphrates and Jeribe Formations in selected wells in Tawke Oil Field, Northwestern Iraq, Zagros-fold belt
Journal of African Earth Sciences,
2023
DOI:10.1016/j.jafrearsci.2023.105000
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[3]
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STRATIGRAPHIC CORRELATION AND SOURCE ROCK CHARACTERISTICS OF THE BALUTI FORMATION FROM SELECTED WELLS IN THE ZAGROS FOLD BELT, KURDISTAN REGION, NORTHERN IRAQ
Journal of Petroleum Geology,
2022
DOI:10.1111/jpg.12806
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[4]
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Determining of dolomitization age and depth of Mardin Group based on clumped isotopes and 1D basin model in SE Anatolia (SE Turkey)
Yerbilimleri/Hacettepe Üniversitesi Yerbilimleri Uygulama ve Araştırma Merkezi Dergisi,
2022
DOI:10.17824/yerbilimleri.1095003
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