This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …

The Arabian Plate originated∼ 25Ma ago by rifting of NE Africa to form the Gulf of Aden and
Red Sea. It is one of the smaller and younger of the Earth's lithospheric plates. The upper …

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 …

The breakup of the supercontinent Gondwanaland into Africa, Antarctica, Australia and India
about 140 million years ago, and consequently the opening of the Indian Ocean, is thought …

Summary The European Plate has a 4.5 Gy long and complex tectonic history. This is
reflected in the present-day large-scale crustal structures. A new digital Moho depth map is …

Seismological models of upper-mantle structure are providing new constraints on the
physical and chemical properties that differentiate the lithosphere from the asthenosphere. A …

The Lesser Caucasus occurs in the hinterland of the Arabia–Eurasia collision zone in the
broad Alpine–Himalayan orogenic belt and includes Cenozoic plutonic and volcanic …

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 …

We present a new digital crustal model for Moho depth and crustal structure in Europe,
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …

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