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The regional geology of Serbia describes the geologic structure and history inside the borders of Serbia. Serbia is in recent geologic time a part of the Eurasian Plate, but the bedrock lithologies are witness to a diverse geologic history. In a tectonic sense, Serbia is part of an orogenic system that is composed of the Alpine, Carpathian, and Dinaride orogenic belts.〔(【引用サイトリンク】title=Structural-Tectonic Elements as a Factor in Cave Development )〕 Its territory can be divided into five geotectonic units of differing genesis: *Pannonian Plain, occupying the northern part of the country (Vojvodina province) *Dinaric Alps occupy western part of Central Serbia, stretching in general northwest-southeast direction *Vardar Zone is a belt east of the Dinaric alps, continuing into central Republic of Macedonia. It consists of three parts: Srem, Jadar and Kopaonik blocks, separated by ophiolitics fractures. *Serbian-Macedonian Massif is a belt stretching in north-south direction along the Great and South Morava valleys, into western Republic of Macedonia and northern Greece (north of Chalkidiki peninsula). *Carpatho-Balkan arc covers Eastern Serbia, in the shape of an arc. Its northern part, Serbian Carpathians is an extension of Carpathian range, and it joins the western parts of Balkan Mountains, whose main massif is in Bulgaria. ==Tectonic units== 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Geology of Serbia」の詳細全文を読む スポンサード リンク
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