Geološki faktori i obeležja rudonosnosti Kaludre (JZ Srbija)

Factors and features of metallization in the Kaludra (SW Serbia)

Abstract

The Kaludra area is geologically restricted to a suit of smaller base-metals ore field inside the tectonized blocks of Senonian flysch in the western Dinarides margin adjoined by the melange of Vardar zone (SW Serbia). Geologic-metallogenic specificities of the Kaludra ore field is attributed to the Tertiary magmatic-tectonic activity, accompanied by penetration of magmatism products and by deposition of postmagmatic mettalized, in essence base-metals complex.

In the paper has been presented the comparative outline and analysis of local controlling geological factors and evidences of metallization. Besides, by its much more widespread distribution, followed by well-expressed correlation with other relevant controlling factors, these are an important element for further prognosis of potential of larger areas in the framework of the ore field.

In the work has been used methodolgy of the synthetized comparative analysis of records of geological prospecting and prognostic analyses of local controlling factors of the mineralization indentification.