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EXPLORATION MINERALISATION AND PERSPECTIVE OF IRON OOLITIC IN REQAK, KOSOVA
Abstract
The territory of our country in terms of cutting geological consists of different geological rocks of all ages from the Quaternary Neoproterozoic up. Magmata’s, and movement of plates that includes the Mediterranean region in earlie r geologic eras led to large-scale geomorphologic and geotect onic reconstruction of the whole region in general and including the region of Kosovo. The impact of these events in the wider region that exceeds the boundaries of our state led to the formation of provinces metallogenetic important for many geological research of the geology specialist for mineralization types of changes related to different geological structures and different types of rocks. In our territory and the vast area surrounding the deposit formed Reqak are significant deposits of useful minerals. Se eing the importance of the use of iron and its vast consumption of the daily needs of his use of alloys, construction and various working mechanisms, the use of mineralization type of iron oolitic character development specific to the country's economy and represents the professional duty to study iron and performances mineralization about deposit and beyond. The purpose of this paper has been the study of several presentations mineralization oolitic iron in the Drenica area with special emphasis on the lo cation of Reqak and determination of the geological characteristics of the studied terrain
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References10
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