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Petrogenetic Characteristics of the Chromite Deposits in Tunceli Province (Turkey).
Date
2015-09-11
Author
Öztüfekçi-önal, Ayten
Çimen, Okay
Toksoy Köksal, Fatma
Aktağ, Alican
Önal, Ali
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https://hdl.handle.net/11511/79341
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Petrogenetic Characteristics of the Chromite Deposits in Tunceli Province Turkey
Öztüfekçi Önal, Ayten; Çimen, Okay; Köksal, Fatma; Aktağ, Alican; Önal, Ali (2015-09-11)
Petrogenesis of Solhan Bingöl volcanics in the East Anatolian Turkey
Oyan, Vural; Özdemir, Yavuz; Keskın, Mehmet; Güleç, Nilgün Türkan (2016-09-05)
Petrogenesis of the Neogene-Quaternary mafic lavas from the Tunceli-Elazığ region (Eastern Turkey)
Aktağ, Alican; Sayıt, Kaan; Department of Geological Engineering (2022-1-27)
The most primitive members of the Late Miocene Tunceli and Pleistocene Elazığ mafic volcanics within the Eastern Anatolian Volcanic Province (EAVP) preserve details regarding the chemical geodynamics of eastern Anatolia. This study, therefore, primarily aims to establish the chemical composition of the source components that have contributed to these volcanics to enhance the understanding of the nature of mantle domains beneath eastern Anatolia. Quantitative modelings suggest that at least three distinct c...
Petrogenesis of alkaline mafic rocks from Sivas, Central Anatolia: New insight into ancient continental assembly and break-up
Pickard, M.; Furman, T.; Kürkcüoğlu, Biltan; Hanan, B.B.; Sayıt, Kaan (2012-06-25)
Petrogenesis and geodynamics of plagiogranites from Central Turkey (Ekecikdag/Aksaray): new geochemical and isotopic data for generation in an arc basin system within the northern branch of Neotethys
Köksal, Serhat; Toksoy Köksal, Fatma; Göncüoğlu, Mehmet Cemal (2017-06-01)
In the Late Cretaceous, throughout the closure of the Neotethys Ocean, ophiolitic rocks from the A degrees zmir-Ankara-Erzincan ocean branch were overthrusted the northern margin of the Tauride-Anatolide Platform. The ophiolitic rocks in the Ekecikdag (Aksaray/Central Turkey) region typify the oceanic crust of the A degrees zmir-Ankara-Erzincan branch of Neotethys. The gabbros in the area are cut by copious plagiogranite dykes, and both rock units are intruded by mafic dykes. The plagiogranites are leucocra...
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A. Öztüfekçi-önal, O. Çimen, F. Toksoy Köksal, A. Aktağ, and A. Önal, “Petrogenetic Characteristics of the Chromite Deposits in Tunceli Province (Turkey).,” 2015, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/79341.
