硅藻是湖泊沉积物的重要组成部分,沉积物硅藻硅氧同位素在重建古气候、古环境方面具有重要价值。
As an important component of lake sediments, diatom is of great value for reconstructing paleoclimate and paleoenvironment.
硅质岩中硅、氧同位素也显示其热水成因之特点。
The Silicon and Oxygen isotopes also demonstrate the characteristics of hydrothermal origin.
硅质岩硅、氧同位素地球化学也显示其热水成因之特点。
The silicon and oxygen isotopes also demonstrate the characteristics of hydrothermal origin.
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