Abstract
Dealing with the problem of the formation and evolution of oceanic and continental crust is one of the fundamental issues in the study of folded areas. The Central Asian fold belt (CAFB), which includes the Dzhida zone of Caledonides, refers to an area where according to some researchers opinions [1–3, etc.], crust forming processes occurred from the Late Riph� ean to the beginning of the Mezozoic. Upon that, as
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