The Low-δ18O Late-Stage Ferrodiorite Magmas in the Skaergaard Intrusion: Result of Liquid Immiscibility, Thermal Metamorphism, or Meteoric Water Incorporation into Magma?
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| Description | scholarly article |
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author: Ilya N. Bindeman |
| Publication date | November 2008 |
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| Missing/wrong data? | Edit Wikidata item |