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 …

Western Anatolia (Turkey) experienced widespread Cenozoic magmatism after the collision
between the Sakarya (SC) and Anatolide–Tauride continental blocks (ATP) in the pre …

Nearly 1500 stress orientation determinations are now available for Europe. The data come
from earthquake focal mechanisms, overcoring measurements, well bore breakouts …

A metamorphic core complex of latest Oligocene age crops out in the Kazdağ mountain
range in northwest Turkey. The footwall of the core complex consists of gneiss, amphibolite …

In northwestern Anatolia two magmatic episodes are distinguished. Initially an intermediate
to felsic calc-alkaline association was formed during the Oligocene-Early Miocene. In this …

The dominant components of Archaean cratonal terrains are tonalitic to trondhjemitic" grey"
gneisses of generally calc-alkaline chemistry but low in K, O. Table 1 lists average …

Post-collisional magmatism in western Anatolia followed a continental collision event in the
Early Eocene, and occurred in discrete pulses that appear to have propagated from north to …

The post-collisional Cenozoic magmatic activity in the Biga Peninsula (NW Anatolia) started
in the Middle Eocene (45.3±0.9 Ma) and lasted continuously until the Late Miocene …

Tertiary-Quaternary magmatism within the Mediterranean and surrounding regions,
including the European foreland of the Alps, the North African margin and the Eastern …

It is known that mineralization in orogenic belts often occurs in extensional settings late in
the collisional history, and without voluminous co-temporal magmatism. In search of the …