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冷水碳酸盐岩沉积
释义
冷水碳酸盐岩沉积
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理学
冷水碳酸盐岩沉积
释
cool-water carbonates
冷水碳酸盐岩沉积
在纬度高于30°~35°的温带及寒带地区、温度低于20℃的沉积水体中,或是在富营养的寒冷上升流水体中形成的碳酸盐沉积物或岩石。
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stability of a singular point
stability of a solution
stability of attention
stability of boundary layer
stability of catalyst
stability of characteristic exponents
stability of colloids
stability of compressed bar
stability of compressible boundary layer
stability of degree two
stability ofdense medium suspension
stability of difference equation
stability of difference equations
stability of difference schemes
stability of differential inclusions
stability of drug crystal form
stability of elastic system
stability of electric circuit
stability of equilibrium of rigid body
stability of equilibrium point
stability of fishing vessel
stability of flight dynamics system
stability of fractional-order systems
stability of gyroscopic systems
stability of hydrides
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