作者hyssop (海索草)
看板EarthScience
标题Re: measuremants of stable isotopes of oxygen..
时间Sun Jul 25 17:32:59 2004
The different content of isotopes (O18/O16) in ice is due primarily to changes
in oceanic and atmospheric temperatures as the lighter isotope of oxygen is
preferentially transferred slowly from the oceans to ice during glaciation
and the rapid transfer back to the ocean during deglaciation.
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