Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …

Integration of regional stratigraphic relationships with data on sediment accumulation,
provenance, paleodrainage, and deformation timing enables a reconstruction of Mesozoic …

We present a map that correlates tectonic units between Alps and western Turkey
accompanied by a text providing access to literature data, explaining the concepts used for …

A new reconstruction of Alpine Tethys combines plate-kinematic modelling with a wealth of
geological data and seismic tomography to shed light on its evolution, from sea-floor …

Construction of the Andes has been governed largely by fluctuating contractional, neutral,
and extensional tectonic regimes during differing degrees of mechanical coupling along the …

Accretionary orogens form at intraoceanic and continental margin convergent plate
boundaries. They include the supra-subduction zone forearc, magmatic arc and back-arc …

A correlation of tectonic units of the Alpine-Carpathian-Dinaridic system of orogens,
including the substrate of the Pannonian and Transylvanian basins, is presented in the form …

Turkey forms one of the most actively deforming regions in the world and has a long history
of devastating earthquakes. The belter understanding of its neotectonic features and active …

A number of tectonic events occurred contemporaneously in the Mediterranean region and
the Middle East 30–25 Myr ago. These events are contemporaneous to or immediately …

The timing of continental collision between the Yangtze and Cathaysia blocks of south
China is an issue that bears on the accretion of Asia, as well as on the assembly and …