| Yazarlar (3) |
Ömer Bozkaya
Pamukkale Üniversitesi, Türkiye |
|
Hüseyin Yalçın
Cumhuriyet Üniversitesi, Türkiye |
Doç. Dr. Zeynel BAŞIBÜYÜK
Kırşehir Ahi Evran Üniversitesi, Türkiye |
| Özet |
| The Sivas Basin is one of the Central Anatolian intracontinental basins. It has been formed on two main continental tectonic units, namely the Tauride-Anatolide Platform in the south and the Central Anatolian Crystalline Complex in the north, during latest Cretaceous-Early Paleocene by the closure of the northern branch of the Neo-Tethys Ocean (eg, Sengör & Yilmaz, 1981; Görür et al., 1998) or as the result of a tensional-transtensional regime (eg, Yilmaz, 1994; Poisson et al., 1996; Dirik et al., 1999). After the evolution of the post-collisional peripheral foreland type of Sivas Basin has been completed during the Middle Miocene by the closure of North Neotethyan ocean and collision of the Anatolian and Arabian plates (eg, Yilmaz, 1994; Poisson et al., 1996; Görür et al., 1998), the shallow intra-cratonic Kangal Basin developed during Middle-Late Miocene onto the Sivas Basin under the neotectonic ova regime (Sengör & Yilmaz, 1981). Kangal Basin consists of fluviatile, lacustrine and/or playa sediments of Middle Miocene-Late Pliocene age. It represents the mineralogical variations corresponding to different facies, and is surrounded by ophiolitic suite (Figure 1). This work reveals the mineralogical and geochemical features of sedimentary rocks and their diagenetic alteration products associated with coal formations and contemporaneous volcanism. |
| Anahtar Kelimeler |
| Bildiri Türü | Tebliğ/Bildiri |
| Bildiri Alt Türü | Tam Metin Olarak Yayınlanan Tebliğ (Uluslararası Kongre/Sempozyum) |
| Bildiri Niteliği | Alanında Hakemli Uluslararası Kongre/Sempozyum |
| Bildiri Dili | İngilizce |
| Kongre Adı | 5th International Symposium on Eastern Mediterranean Geology (5th ISEMG) |
| Kongre Tarihi | 14-04-2004 / 20-04-2004 |
| Basıldığı Ülke | |
| Basıldığı Şehir |
