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Partitioning of trace elements between crystals and melts
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“While primitive (unmodified) mantle (PM) has its own unique Nb/Th and Zr/Nb ratios, these signatures do not show up in basalt melt fractions unless by chance, given crystal–melt partitioning during the mantle melting process (Blundy and Wood, 2003).”
Background
Metadata
- Authors
- Blundy, J., & Wood, B.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2003-05
- Volume
- 210
- Issue
- 3-4
- Pages
- 383-397
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W1963901012
- Cited by
- 470
- References
- 3
- FWCI
- 13.80
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.elsevier.com/tdm/userlicense/1.0/ (tdm)
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