Granites – Depth, pickle magmatic rocks and in the Earth’s crust appear as large geological bodies, usually batolites or digits. After its genesis can be and types, when they occur with the differentiation of the basaltoid magma in island arches and s-types, when they arise as a result of the partial melts of the deep parts of the continental crust. The granites are built of quartz, cali feldspar, lish and accelerine minerals. The color is different and depends on the present minerals. The structure is most often grainy, but there are porphyroid varieties. On the territory of the Republic of Macedonia are widespread and has in all geotectral units. After old age, they appear from the prelimbibrist until the tertiary. The oldest granites appear in the Pelagonia metamorphic complex and their age is about 1 billion years, and the youngest appear in the Vardar zone and their age is about 32 million years. Ⅹⅴⅰⅰ Cowresis OF Tsarphartian-Balkan Geologic Associatic, Bratislava, 2002. BL. B. Scene from the documentary film “Border”
Original article in Macedonian language Cyrillic alphabet
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