Foreland Magmatism during the Arabia–Eurasia Collision: Pliocene–Quaternary Activity of the Karacadağ Volcanic Complex, SW Turkey

Abstract

Pliocene to Quaternary magmatism in the Karacada! g Volcanic Complex in SE Turkey occurred in the foreland region of the Arabia^Eurasia collision and can be divided into two phases. The earlier Karacada! g phase formed a north^south-trending volcanic ridge that erupted three groups of lavas. The same range of mantle