This global study of 31 off-shore back-arc basins and subbasins (BABs) identifies their
principal characteristics based on a broad spectrum of geophysical and subduction-related …

The deformation of Earth's lithosphere in orogenic belts is largely forced externally by the
sinking slab, but can also be driven by internal delamination processes caused by …

The third edition of this widely acclaimed textbook provides a comprehensive introduction to
all aspects of global tectonics, and includes major revisions to reflect the most significant …

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 …

Post-collisional magmatism in western Anatolia began in the Eocene, and has occurred in
discrete pulses throughout the Cenozoic as it propagated from north to south, producing …

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 …

An east–west trending, high-density seismic array was deployed along the eastern margin of
the Tibetan Plateau to investigate its eastward expansion. The 160 km long array spans the …

We use the tephrostratigraphic framework along the Aegean Volcanic Arc established in
Part 1 of this contribution to determine hemipelagic sedimentation rates, calculate new …

We place the geological history since Cretaceous times in western Turkey in a context of
convergence, subduction, collision and slab break-off. To this end, we compare the west …

Combined P and S receiver functions from seismograms of teleseismic events recorded at
65 temporary and permanent stations in the Aegean region are used to map the geometry of …