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冷水碳酸盐岩沉积
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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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