Across the entire mantle we interpret 94 positive seismic wave-speed anomalies as
subducted lithosphere and associate these slabs with their geological record. We document …

We review the geodynamic evolution of the Aegean–Anatolia region and discuss strain
localisation there over geological times. From Late Eocene to Present, crustal deformation in …

Seismic tomography models of the three-dimensional upper mantle velocity structure of the
Mediterranean-Carpathian region provide a better understanding of the lithospheric …

Metamorphic belts are complex regions where accretion or collision has added to, or
thickened, continental crust. Gold-rich deposits can be formed at all stages of orogen …

The Aegean region is a concentrate of the main geodynamic processes that shaped the
Mediterranean region: oceanic and continental subduction, mountain building, high …

Slab edges are a relatively common feature in plate tectonics. Two prominent examples are
the northern end of the Tonga subduction zone and the southern end of the New Hebrides …

Lithospheric deformation throughout Anatolia, a part of the Alpine–Himalayan orogenic belt,
is controlled mainly by collision-related tectonic escape of the Anatolian Plate and …

There are six distinct classes of gold deposits, each represented by metallogenic provinces,
having 100's to> 1000 tonne gold production. The deposit classes are:(1) orogenic gold;(2) …

The Cenozoic history of the retreating Hellenic subduction system in the eastern
Mediterranean involves subduction, accretion, arc magmatism, exhumation, normal faulting …

Archean orogenic lode gold deposits are the result of large, complex mineralizing systems
that have developed within many Archean terrains. Mineralizing systems are defined to …