In a huge block within the
Latest Cretaceous volcanic olistostrome Unit in the Izmir-Ankara zone,
nonmetamorphic epidastic and carbonate Late Triassic (Carnian) strata rest
unconformably on metacarbonate. Abundant sand-sized detritus of serpentinite
occur in the Late Triassic strata. The unconformity is comparable, with respect
to stratigraphic setting, with that in the northerly-lying Late Triassic
turbidite-olistostrome zone, between the low-grade metamorphic basement and the
Late Triassic sedimentary cover.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Ekim 1995 |
Yayımlandığı Sayı | Yıl 1995 Cilt: 117 Sayı: 117 |
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