2003-02
AUTHORS ABSTRACTIsotope data provide insight into the earliest phases of terrestrial evolution. The latest reappraisal supports the view that the early Earth had a cratered crust which crystallized from a magma ocean.
PAGES901-903
http://scigraph.springernature.com/pub.10.1038/421901a
DOIhttp://dx.doi.org/10.1038/421901a
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PUBMEDhttps://www.ncbi.nlm.nih.gov/pubmed/12606982
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