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Apatite fission-track (FT) ages from the Central Anatolian Crystalline Complex (CACC), a microcontinent within the Turkish segment of the Alpine-Himalayan orogen, vary dramatically from north to south. This variation correlates with differences in the obliquity of convergence of the continental fragment relative to the Pontide belt (for the northern CACC) and the Tauride belt (for the southern CACC)...
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