Paleontology and Stratigraphy of Fossils

Abstract. Iron is a key micronutrient for phytoplankton growth in the surface ocean. Yet the significance of volcanism for the marine biogeochemical iron-cycle is poorly constrained. Recent studies, however, suggest that offshore deposition of airborne ash from volcanic eruptions is a way to inject significant amounts…

• NAZLI OLĞUN KIYAK

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• MEHMET ORUÇ BAYKARA

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• ALİ GÖKGÖZ

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• MEHMET CİHAT ALÇİÇEK

In the Denizli Basin (Turkey), located in the western Anatolian extensional province, travertine and tufa deposition has been an ongoing process for at least 600,000 years. Travertine bodies, which are 30 to 75 m thick and each covers areas of 1 to 34 km2, are up to 1 km3 in volume. Today, spring waters in this area h…

• MEHMET ORUÇ BAYKARA

In the Denizli Basin (Turkey), located in the western Anatolian extensional province, travertine and tufa deposition has been an ongoing process for at least 600,000 years. Travertine bodies, which are 30 to 75 m thick and each covers areas of 1 to 34 km2, are up to 1 km3 in volume. Today, spring waters in this area h…

• MEHMET CİHAT ALÇİÇEK

In the Denizli Basin (Turkey), located in the western Anatolian extensional province, travertine and tufa deposition has been an ongoing process for at least 600,000 years. Travertine bodies, which are 30 to 75 m thick and each covers areas of 1 to 34 km2, are up to 1 km3 in volume. Today, spring waters in this area h…

• ALİ GÖKGÖZ

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• GÜLTEKİN TOPUZ

Summary In this paper we describe and interpret a critical segment of a Tethyan suture zone in SE Turkey dominated by a major nappe pile which, from the structural top downwards, consists of the following units: first, the Elazıǧ-Palu nappe , a major Upper Cretaceous volcanic arc complex and cover related to subducti…

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• GÜLTEKİN TOPUZ

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