Collisional and post-collisional volcanic rocks in the Ulubey (Ordu) area at the western edge
of the Eastern Pontide Tertiary Volcanic Province (EPTVP) in NE Turkey are divided into four …

The major and trace elements and Sr–Nd–Pb isotopes of the host rocks and the mafic
microgranular enclaves (MME) gathered from the Dölek and Sariçiçek plutons, Eastern …

Crustal and upper-mantle seismic discontinuities beneath eastern Turkey are imaged using
teleseismic S-to-P converted phases. Three crustal phases are observed: the Moho with …

Eastern Anatolia is one of the best examples of an active continental collision zone in the
world. It comprises one of the high plateaus of the Alpine-Himalaya mountain belt, with an …

The Eocene volcano-sedimentary units of Northern Anatolia are confined into a narrow zone
trending parallel to the Intra Pontide and İzmir–Ankara–Erzincan sutures, along which the …

The continental arc and intraplate magmatic rocks occur widely within the Altun-Qilian-North
Qaidam (AQNQ) region of NW China and play a key role in reconstructing the assembly and …

The core of Turkey's land is the Anatolian Peninsula, which is surrounded by several seas
(Mediterranean, Aegean, Marmara and Black Sea). Offering a high variety of morphological …

Quaternary mafic lavas in Central Anatolia provide geochemical insights into melt
generation processes following regional delamination of the subducted Tethyan slabs. New …

A 3-D upper-mantle structure beneath Turkey is investigated using phase speeds of
fundamental-mode Rayleigh waves employing a conventional two-station method with high …

Abstract The Variscan Orogen in Iberia and the Anti-Atlas Mountains in Morocco contains a
set of ophiolites formed between Neoproterozoic and Devonian times, during the complex …