Henry's law behavior in simple systems and in magmas: Criteria for discerning concentration-dependent partition coefficients in nature

Author:

Watson E.Bruce

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference21 articles.

1. The partition of Sr, Ba, Ca, Y, Eu2+, EU3+, and other REE between plagioclase feldspar and magmatic liquid: an experimental study;Drake;Geochim. Cosmochim. Acta,1975

2. “Henry's law” behaviour of Sm in a natural plagioclase/melt system: importance of experimental procedure;Drake;Geochim. Cosmochim. Acta,1978

3. Partitioning of Ni between olivine and silicate melt: the ‘Henry's law problem’ reexamined;Drake;Geochim. Cosmochim. Acta,1981

4. Partition coefficients of Hf, Zr, and REE between phenocrysts and ground-masses;Fujimaki,1984

5. Partitioning of REE between minerals and coexisting melts during partial melting of a garnet lherzolite;Harrison;Amer. Mineral.,1981

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