Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi
Yıl: 2022 Cilt: 43 Sayı: 3 Sayfa Aralığı: 212 - 238 Metin Dili: Türkçe DOI: 10.17824/yerbilimleri.1095003 İndeks Tarihi: 16-01-2023
Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi
Öz: Güneydoğu Anadolu Bölgesi’nde geniş bir yayılım sergieyen Kretase yaşlı sığ denizel Mardin Grubu karbonatları hidrokarbon açısından en üretken birimdir. Mardin Grubu dolomitlerinin kümelenmiş izotop sıcaklıkları 92 oC ile 125 oC arasında ölçülmüştür. Bir boyutlu (1B) basen modeli kullanılarak, kümelenmiş izotop sıcaklıkları dolomitleşme derinlik ve zaman bilgisine dönüştürülmüş ve dolomitleşmenin 2200 m derinlikten (22 milyon yıl önceden- Erken Miyosen) 3420 m derinliğe (14 milyon yıl önceye kadar- Orta Miyosen) kadar gerçekleştiği anlaşılmıştır. Düşük Fe ve Mn element konsantrasyonları dolomitleşme sularının denizel kökenli olduğunu işaret ederken, 200 ppm’den daha düşük değerler alan Sr element sonuçları ise geç evre dolomitleşmenin olduğunu göstermektedir. Geç diyajenez boyunca paleo-sıcaklık ve derinlik değerlerinin değişimi yeniden kristallenmenin farklı derecelerde meydana geldğini yansıtmaktadır. Dolomitleşme sularının oksijen izotop değerleri %3.32 ve %6.31 arasında değişmektedir. Bu değerler Kretase deniz sularından izotopik olarak daha ağırdırlar. Sonuçlar gösteriyor ki, çalışma alanında geç dolomitleşme olayı gözlemlenmekte ve yüksek sıcaklıktaki derin gömülmüş ve dolomitleşme ile oluşmuş gözenek suları Mardin Grubu rezervuarının porozite sistemini olumsuz yönde etkilemektedir.
Anahtar Kelime: Determining of Dolomitization Age and Depth of Mardin Group Based on Clumped Isotopes and 1D Basin Model in SE Anatolia (SE Turkey)
Öz: The widespread Cretaceous aged Mardin Group is shallow marine carbonates and is the most proliferous section in SE Anatolia (SE Turkey). Clumped isotope temperatures were measured for Mardin dolomites between 92 oC and 125 oC. Using 1D basin model, clumped isotopes temperatures were converted to a depth and time for dolomitization from 2200 m (22 Ma-Early Miocene) to 3420 m (14 Ma-Middle Miocene). While low Fe and Mn concentration reflects marine fluids as a dolomitizing water, Sr values less than 200 ppm shows existence of late diagenesis. Both the range of paleotemperature and burial depth reflects different degree of recrystalization event as a result of burial event. The oxygen isotopic composition of dolomitizing fluid varied between 3.32% and 6.31% which is isotopically heavier than Cretaceous marine waters. The results indicates that late dolomitization are present in the study area and that a deeply buried dolomitizing pore fluid with high T has a negative influence on porosity system of the Mardin Group Reservoir.
Anahtar Kelime: Belge Türü: Makale Makale Türü: Araştırma Makalesi Erişim Türü: Erişime Açık
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| APA | atasoy d, Büyükutku A, Geçer A, AKTOSUN A (2022). Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. , 212 - 238. 10.17824/yerbilimleri.1095003 |
| Chicago | atasoy deniz,Büyükutku Aynur,Geçer Aylin,AKTOSUN ARZU Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. (2022): 212 - 238. 10.17824/yerbilimleri.1095003 |
| MLA | atasoy deniz,Büyükutku Aynur,Geçer Aylin,AKTOSUN ARZU Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. , 2022, ss.212 - 238. 10.17824/yerbilimleri.1095003 |
| AMA | atasoy d,Büyükutku A,Geçer A,AKTOSUN A Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. . 2022; 212 - 238. 10.17824/yerbilimleri.1095003 |
| Vancouver | atasoy d,Büyükutku A,Geçer A,AKTOSUN A Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. . 2022; 212 - 238. 10.17824/yerbilimleri.1095003 |
| IEEE | atasoy d,Büyükutku A,Geçer A,AKTOSUN A "Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi." , ss.212 - 238, 2022. 10.17824/yerbilimleri.1095003 |
| ISNAD | atasoy, deniz vd. "Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi". (2022), 212-238. https://doi.org/10.17824/yerbilimleri.1095003 |
| APA | atasoy d, Büyükutku A, Geçer A, AKTOSUN A (2022). Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. Yerbilimleri, 43(3), 212 - 238. 10.17824/yerbilimleri.1095003 |
| Chicago | atasoy deniz,Büyükutku Aynur,Geçer Aylin,AKTOSUN ARZU Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. Yerbilimleri 43, no.3 (2022): 212 - 238. 10.17824/yerbilimleri.1095003 |
| MLA | atasoy deniz,Büyükutku Aynur,Geçer Aylin,AKTOSUN ARZU Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. Yerbilimleri, vol.43, no.3, 2022, ss.212 - 238. 10.17824/yerbilimleri.1095003 |
| AMA | atasoy d,Büyükutku A,Geçer A,AKTOSUN A Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. Yerbilimleri. 2022; 43(3): 212 - 238. 10.17824/yerbilimleri.1095003 |
| Vancouver | atasoy d,Büyükutku A,Geçer A,AKTOSUN A Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi. Yerbilimleri. 2022; 43(3): 212 - 238. 10.17824/yerbilimleri.1095003 |
| IEEE | atasoy d,Büyükutku A,Geçer A,AKTOSUN A "Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi." Yerbilimleri, 43, ss.212 - 238, 2022. 10.17824/yerbilimleri.1095003 |
| ISNAD | atasoy, deniz vd. "Güneydoğu Anadolu Bölgesi Mardin Grubu Dolomitlerinin Dolomitleşme Yaşlarının ve Derinliklerinin Kümelenmiş İzotoplar ve 1B Basen Modeli Kullanılarak Belirlenmesi". Yerbilimleri 43/3 (2022), 212-238. https://doi.org/10.17824/yerbilimleri.1095003 |
