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Eclogitic diamonds from variable crustal protoliths in the northeastern Siberian craton: Trace elements and coupled δ13C-δ18O signatures in diamonds and garnet inclusions
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文摘

New data of δ18O of garnet inclusions and δ13C of host diamonds are presented.

The relationship between δ18O of E-type Grts and δ13C of host diamonds is confirmed.

The variability of E-type Grts is inherited from contrasting crustal protoliths.

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