Minor phases as Carriers of trace elements in non-modal crystal-liquid separation processes II: Illustrations and bearing on behaviour of REE, U, Th and the PGE in igneous processes

Journal of Petrology

Volumn 42, Issue 10, 2001, Pages 1887-1910

  O'Hara, M J ^a   Fry, N ^a   Prichard, H M ^a  

^a CARDIFF UNIVERSITY   (United Kingdom)

Author keywords

Chromite; Distribution coefficient; Platinum; Sulphide; Uranium

Indexed keywords

CHROMITE; FRACTIONAL CRYSTALLIZATION; IGNEOUS GEOCHEMISTRY; MELTING; PLATINUM GROUP ELEMENTS; SULFIDE; URANIUM;

EID: 0034776429     PISSN: 00223530     EISSN: None     Source Type: Journal    
DOI: 10.1093/petrology/42.10.1887     Document Type: Article

References (18)

1. Experimental determination of REE distributions between monazite and xenotime: Potential for temperature calibrated geochronology
2. Chronology and mechanism of depletion in Lewisian granulites
3. Origin of chromite layers in the Muskox intrusion and other stratiform intrusions: A new interpretation
4. Geochemical consequences of in situ crystallisation
5. Association of platinum-group elements with chromitite in layered intrusions and ophiolite complexes
6. Geochemical evolution during fractional crystallization of a periodically refilled magma chamber
7. Importance of the 'shape' of the melting regime during partial melting of the mantle
8. Trace element geochemical effects of imperfect crystal-liquid separation
9. Trace element geochemical effects of integrated melt extraction and 'shaped' melting regimes
10. The highly compatible trace element paradox-fractional crystallization revisited
11. Geochemical effects of small packet crystallization in large magma chambers-further resolution of the highly compatible element paradox
12. 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
13. Geochemical evolution in an advancing, periodically replenished, periodically tapped, continuously fractionated magma chamber
14. High pressure-temperature reference point on an Archaean geotherm, implied magma genesis by crustal anatexis and consequences for garnet-pyroxene thermometry and barometry
15. Minor phases as carriers of trace elements in non-modal crystal-liquid separation processes I: Basic relationships
16. Effects of the melting regime on the composition of the oceanic crust
17. Abyssal tholeiites from the Oceanographer fracture zone II: Phase equilibria and mixing