English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Zendy Plus

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Zendy Tools

Zendy Open

Partial melting of natural rocks is likely to proceed with the pooling of liquids which have been produced by a range of mass fractions of liquid development ( O'Hara, 1985 , 1995 ; Richter, 1986 ; Langmuir, 1989 ; Eggins, 1992 ; Plank &amp; Langmuir, 1992 ; O'Hara &amp; Fry, 1996 ). Partial crystallization of magmas in magma chambers may involve the integration of residual liquids from a range of mass fractions of liquid survival either through the crystallization zone or across the crystallizing surface ( Langmuir, 1989 ; O'Hara &amp; Fry, 1996 ). The concentrations of ideally behaved trace elements in an integrated liquid or solid and that in the product of a simple process operating at the same average mass fraction of liquid in the system are, in general, significantly different ( O'Hara, 1995 ; O'Hara &amp; Fry, 1996 ). However, under the highly selected and simplified conditions reviewed here, the results of integrating the liquids and solids produced in simple fractional melting or crystallization models are formally identical at all values of the distribution coefficient to the product of a simple equilibrium process at the average mass fraction of melt or residual liquid.

journal of petrology

Integrated Compositions of Perfect Fractional Liquid and Solid Products are Identical, with Respect to Ideal Trace Element Behaviour, to Simple Equilibrium (Batch) Products in Very Special Cases