Cobalt and scandium partitioning versus iron content for crystalline phases in ultramafic nodules

Earth and Planetary Science Letters

Volumn 39, Issue 1, 1978, Pages 173-178

  Glassley, W E ^a   Piper, D Z ^b  

^a MIDDLEBURY COLLEGE   (United States)

^b U S GEOLOGICAL SURVEY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0004997622     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/0012-821X(78)90153-X     Document Type: Article

References (15)

1. Trace element partitioning between two pyroxenes and the host lava
2. Trace element partitioning between volcanic plagioclases and dacitic pyroclastic matrix
3. Factors affecting element ratios in the crystallization of minerals
4. Origin of the garnet pyroxenite xenoliths at Salt Lake Crater, Oahu
5. Xenoliths in the Honolulu volcanic series, Hawaii
6. Garnet-orthopyroxene and orthopyroxene-clinopyroxene relationships in simple and complex systems
7. 3+, and other REE between plagioclase feldspar and magmatic liquid; an experimental study
8. Scandium
9. Crystal chemistry of iron
10. 6
11. Patterns of trace element partitioning
12. Kinetic disequilibrium in trace element partitioning between phenocrysts and host lava
13. The character of the lower crust and upper mantle beneath the Hawaiian Islands
14. Phenocryst matrix partition coefficients for K, Rb, Sr and Ba, with applications to anorthosite and basalt genesis
15. Problems in determining mantle geotherms for pyroxene compositions of ultramatic rocks