Trace element analyses of magnetites from andesitic and dacitic lavas from Bay of Plenty, New Zealand
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/BF00371064.pdf
Reference7 articles.
1. Burns, R. G., and W. S. Fyfe: Site preference energy and selective uptake of transition-metal ions from a magma. Science 144, 1001?1003 (1964).
2. Ewart, A., S. R. Taylor, and A. C. Capp: Trace and minor element geochemistry of the Rhyolitic Volcanic Rocks, Central North Island, New Zealand. Total rock and residual liquid data. Contr. Mineral. and Petrol. 18, 76?104 (1968).
3. Osborn, E. F.: Reaction series for subalkaline igneous rocks based on different oxygen pressure conditions. Am. Mineralogist 47, 211?226 (1962).
4. Roeder, P. L., and E. F. Osborn: Fractional crystallisation trends in the system Mg2SiO4-CaAl2Si2O8-FeO-Fe2O3-SiO2 over the range of oxygen partial pressures of 10?11 to 10?0,7 atm. Bull. volcanol. 29, 659?668 (1966a).
5. ?: Experimental data for the system MgO-FeO-Fe2O3-CaAl2Si2O8-SiO2 and their petrological implications. Am. J. Sci. 264, 428?480 (1966b).
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