Based on the two-dimension adlittoral non-invariablenes flow control equation of lakes,a hydrodynamic model of lakes was built up.
从二维浅
非恒定流
控制方程出发,建立了一个二维湖泊流体动力学模型。
Based on the two-dimension adlittoral non-invariablenes flow control equation of lakes,a hydrodynamic model of lakes was built up.
从二维浅
非恒定流
控制方程出发,建立了一个二维湖泊流体动力学模型。
10.basement and unmetamorphosed terrigenous shallow carbonate rock in the Austria Alps -South Alps obduc-tion nappe and radiolarian silicalite in fault basins.
奥地利阿

—南阿

仰冲叠覆体中
基底和未受变质
南大陆边缘
浅
碳酸盐岩及断
盆地内较
放射虫硅质岩。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆积了从陆相到海相,从浅
到

各种沈积体系,组成向上变细和变
充填序列。
It was only a bayou in the ancient time and later on it became a lake for the tide had brought sand to the bayou.After numerous constructions, it became a semi-closed adlittoral lake.
古时为一海湾,因江潮挟带泥沙长期堆积形成“泻湖”,又经过历代不断疏浚建设而成为半封闭
浅
湖泊。
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