The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

Changing components, rock textures, lithofacies, platform types and architecture throughout
time are unique characteristics of carbonate rocks. Characterizing these attributes has been …

The carbonate factories model, as defined at the beginning of the century, provides a
subdivision of marine carbonate sediment production‐systems based on the style of …

Abstract The Central and Eastern Anatolian plateaus are integral parts of the world's third
largest orogenic plateau. In the past decade, geophysical surveys have provided insights …

Valid palaeotectonic and palaeogeographical reconstructions of the easternmost
Mediterranean and adjacent region involve a long-lived Tethys (Rheic, Palaeotethyan and …

Uplifted Neogene marine sediments and Quaternary fluvial terraces in the Mut Basin,
southern Turkey, reveal a detailed history of surface uplift along the southern margin of the …

The timing and pattern of surface uplift of Miocene marine sediments capping the southern
margin of the Central Anatolian Plateau in southern Turkey provide a first-order constraint on …

Miocene is a key interval in the global climate evolution as well as in the geodynamic
evolution of the Mediterranean basin. Therefore, global and regional factors controlled …

Shallow-marine tidal deposits form on open shelves, and more specifically in open-mouthed
embayments and semi-enclosed epicontinental seas, where the oceanic tide is amplified by …

The spectrum of carbonate-platform types, their heterogeneities, and their architecture is
complex. Each platform succession has a distinctive and unique character that is a response …