Mantle refertilization in high-pressure conditions of continental subduction channel:Evidence from orogenic peridotite in the Sulu ultrahigh pressure terrane, eastern China
التفاصيل البيبلوغرافية
العنوان:
Mantle refertilization in high-pressure conditions of continental subduction channel:Evidence from orogenic peridotite in the Sulu ultrahigh pressure terrane, eastern China
Figure S1a illustrates the comparison between the Grt/Cpx partition coefficients of garnet lherzolite (Chijiadian) and experiment data. Figure S1b calculates the REE compositions of metasomatic melts. Figure S1a illustrates the comparison between the Grt/Cpx partition coefficients of garnet lherzolite (Chijiadian) and experiment data. Figure S1b calculates the REE compositions of metasomatic melts. Tables S1 to S3 supply the major and trace elements of bulk rock and minerals, as well as Sr isotopes in situ used in this article. Table S4 gives the partition coefficients related to the calculations of Figure S1.
