Abstract:Lacustrine basins of Neogene age in Serbia which were formed in intramountain valleys, graben-like structures (mostly half graben) are characterized by the occurrences of alluvial,swamp and lacustrine factes and subfacies.
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释义
塞尔维亚新第三纪湖泊盆地是形成于山间河谷中的具地堑状(大部是半地堑状)构造的盆地,其特征是有冲积、沼泽和湖相与亚相。
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