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Published in 2020 at "Earth and Planetary Science Letters"
DOI: 10.1016/j.epsl.2020.116331
Abstract: Abstract The δ 18 O value of seawater is presently buffered by high-temperature hydrothermal alteration and low-temperature weathering of lithospheric rocks. It is much debated whether the δ 18 O of seawater has been buffered…
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Keywords:
seawater;
oxygen isotope;
value;
archean seawater ... See more keywords