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

Journal of Petrology

Volumn 38, Issue 3, 1997, Pages 425-430

  O'Hara, M J ^a   Fry, N ^a  

^a CARDIFF UNIVERSITY   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0000235998     PISSN: 00223530     EISSN: None     Source Type: Journal    
DOI: 10.1093/petroj/38.3.425     Document Type: Article

References (7)

1. Eggins, S. M., 1992. Petrogenesis of Hawaiian tholeiites: 2, aspects of dynamic melt segregation. Contributions to Mineralogy and Petrology 110, 398-410.
2. Langmuir, C. H., 1989. Geochemical consequences of in situ crystallisation. Nature 340, 199-205.
3. O'Hara, M. J., 1985. Importance of the 'shape' of the melting regime during partial melting of the mantle. Nature 314, 58-62.
4. O'Hara, M. J., 1995. Trace element geochemical effects of integrated melt extraction and 'shaped' melting regimes. Journal of Petrology 36, 1111-1132.
5. O'Hara, M. J. & Fry, N., 1996. The highly compatible trace element paradox - fractional crystallization revisited. Journal of Petrology 37, 859-890.
6. Plank, T. & Langmuir, C. H., 1992. Effects of the melting regime on the composition of the oceanic crust. Journal of Geophysical Research 97, 19749-19770.
7. Richter, F. M., 1986. Simple models for trace element fractionation during melt segregation. Earth and Planetary Science Letters 77, 333-344.