Geochemical Analyses in Mineral Deposits ' ?ikatova e Vjeter' in Drenas Area-Kosovo

摘要

Mineral deposit .ikatova e Vjeter consists of two ore bodies that are laterites process iron-nickel products of weathering crust developed in ultrabasic rocks. Dushkaja ore body present Nicel-Iron silicate product of weathering crust coverage primary type formed up serpentenites. Ore body Suka is typical resedimentation Quaternary deposits of Iron- Nickel laterite consists of four lentils with irregular shapes unrelated to each other and is located south of Dushkaja distance of 800 m. Studies have determined different vertical zonality in weathering crust of ore body Dushkaja and Suka which are separate zones with geochemical characteristics. Content of nickel in ore body "Suka" compared with Ni in Dushkaja not show any significant poorer. Mineral deposits Cikatova e Vjeter is locating in Drenas region Kosovo territory. The paper aims thanks of metalogeny analyse to clarify and define the main geology conditions nickel ore forming deposits in time and space in the territory of Kosovo and defining criteria for research and finding of new metalogeny units with iron- nickel ore.