Tree rings and seasonal sedimentary deposits called varves can be counted to determine absolute age.
可以树木
轮和被称为纹泥
季节性沉积物进行计数来确定其绝
。
Tree rings and seasonal sedimentary deposits called varves can be counted to determine absolute age.
可以树木
轮和被称为纹泥
季节性沉积物进行计数来确定其绝
。
The variation of varve thickness may show a decrease of sediment flux during the Little Ice Age, and an increase of sediment flux after 1960s.
但纹层厚度变化可能揭
冰期沉积通量
减少和上个世纪六十
代之后沉积通量
增加。
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