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by
Williams, Dustin, author.
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in-situ fractional crystallization at intermediate to low magmatic temperatures and record the pre
by
Duccini, Kalie, author.
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crystallization in the deep crust. Evidence for dissolution and reequilibration in early-formed minerals suggests
by
Drumm, Stephanie M., author.
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structures. The USF and EarthChem samples were then compared to various crystallization models generated in
by
Freeman, Zachary William, author.
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consistent with fractional crystallization. These results indicate that AAIP olivines are phenocrysts rather
by
Benson, Erin, author. (orcid)0000-0003-3166-6043
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the magma crystallization sequence, before Ni was sequestered by olivine. This strongly indicates that





