Trace element partitioning between majoritic garnet and silicate melt at 10-17 GPa: Implications for deep mantle processes

No abstract is available for this paper.

• Publication year

  2012

• Venue

  Lithos

• Publication date

  2012-09-01

• Fields of study

  Geology

• Identifiers
  DOI 10.1016/J.LITHOS.2012.06.013
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

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