ɪnðɪ ˈɜːli kˌɑːɹbənˈɪfɚɹəs haʊˈɛvɚ, ɐ sʌbdˈʌkʃən zˈoʊn dɪvˈɛləpt sˈaʊθ ʌvðə jˌʊɹɹəpˈiən hjˈuːnɪk tˈɛɹeɪnz kənsˈuːmɪŋ pˈeɪlɪˌoʊtˈɛθiz ˌoʊʃɪˈænɪk kɹˈʌst.
In the Early Carboniferous however, a subduction zone developed south of the European Hunic terranes consuming Paleo-Tethys oceanic crust.