Abstract The Central Anatolian Plateau (CAP) in Turkey is a relatively small plateau (300× 400 km) with moderate average elevations of∼ 1 km situated between the Pontide and …
Mean coral cover has reportedly declined by over 15% during the last 30 years across the central Great Barrier Reef (GBR). Here, we present new data that documents widespread …
Much remains to be understood about the links between regional vertical axis rotations, continental extension, and shortening. In western Turkey, Miocene vertical axis rotations …
Abstract The Hellenic and Cyprus Arcs, that mark the convergent boundary of the African and Aegean–Anatolian plates, are offset along a subduction transform edge propagator …
Stony corals, especially scleractinians, are a recurrent component of the benthic fauna of the Mediterranean basin and its Mesozoic-to-Cenozoic precursors. Both morphological and …
During the Oligocene–Miocene Greenhouse-to-Icehouse climatic transition, the biogeography of reef corals or zooxanthellate-like scleractinian corals was gradually …
The Eşen Basin of southwestern Anatolia formed as a NE-trending intramontane extensional graben, ca. 15 km wide and 30 km long, in the Early Tortonian, after the southeasterly …
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 …
Toros Karst Kuşağı'nın karakteristik yerşekillerinden olan polyeler, en geniş ve görece en karmaşık karstik yüzey şekillerindendir. Polyeler Anadolu'da en fazla çalışılmış …