The early Paleogene experienced the most pronounced long-term warming trend of the
Cenozoic, superimposed by transient warming events such as the Paleocene–Eocene …

According to the prevailing view in literature, two Eocene carbonate platform belts
developed on northern and southern margins of the Tethys Ocean. However, Eocene …

Abstract Before the Late Cretaceous opening of the Black Sea, the Central Pontides
constituted part of the southern margin of Laurasia. Two features that distinguish the Central …

A paleoecological and sedimentological study was carried out on shallow-water carbonates
of the Kras Plateau (SW Slovenia) with the goal of reconstructing paleoenvironmental …

The Paleocene–Early Eocene carbonate successions of the Indus Basin in Pakistan formed
on the northwestern continental shelf margin of the Indian Plate in the eastern Tethys Ocean …

The succession of the Galala Mountains at the southern Tethyan margin (Eastern Desert,
Egypt) provides new data for the evolution of an isolated carbonate platform in the Early …

We present an integrated, high-resolution, biostratigraphical, mineralogical, and
geochemical characterization of the well-exposed Upper Paleocene-Lower Eocene …

Maastrichtian to Paleocene shallow-water carbonate rocks are common in many parts of
Turkey. The occurrence of the Şahinkaya Member limestones in the Çayırbağı-Çalköy …

Abstract The Central Pontides of N Turkey represents a mobile orogenic belt of the southern
Eurasian margin that experienced several phases of exhumation associated with the …

The geodynamic evolution of Turkey is mainly controlled by drift and collision of a number
oceanic and continental plates or terranes. This can be ascribed to four orogenic episodes …