Tree rings and seasonal sedimentary deposits called varves can be counted to determine absolute age.
可以对树木的轮和被称为纹泥的沉积物进行计数来确定其绝对龄。
Tree rings and seasonal sedimentary deposits called varves can be counted to determine absolute age.
可以对树木的轮和被称为纹泥的沉积物进行计数来确定其绝对龄。
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.
但纹层厚度的化可能揭示出小冰期沉积通量的减少和上个世纪代之后沉积通量的增加。
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