Dağküplü ophiolithic complex which is situated around Yakakayı-Gündüzler villages to the north of Eskişehir
indicates southerly overturned structural position. Mesozoic ophiolithic rocks, from bottom to top present a sequence of ophiolithic
melange, mafic and ultramafic cumulates and tectonites. Cumulate sequence begins with gabbroes at the bottom passes to
the dunite interlayered pyroxenites towards to the top.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Şubat 1989 |
Yayımlandığı Sayı | Yıl 1989 Cilt: 109 Sayı: 109 |
Copyright and Licence
The Bulletin of Mineral Research and Exploration keeps the Law on Intellectual and Artistic Works No: 5846. The Bulletin of Mineral Research and Exploration publishes the articles under the terms of “Creatice Common Attribution-NonCommercial-NoDerivs (CC-BY-NC-ND 4.0)” licence which allows to others to download your works and share them with others as long as they credit you, but they can’t change them in any way or use them commercially.
For further details;
https://creativecommons.org/licenses/?lang=en