Variscan (Upper Carboniferous 370-290Ma) Magmatic Arc in Western Rhodope, as segment of the well known Tethyan Metallogeny Belt of Europe (Porphyry Cu-Au and Epithermal Au-Ag belt)
Regionally the same Variscan magmatic arc extends from Czech Republic, through central Bulgaria and further east to Kazakhstan and south Mongolia
That belt is developed along the active continental margin of the Eurasia continent characterized by a number of reduced gold and tungsten bearing hydrothermal systems that produced some of the world class gold deposits (Czech Republic, Bulgaria and Kazakhstan) associated with many tungsten and molly manifestations in Slovakia, Austria and Bulgaria