Major and trace element zoning in plagioclase from Kizimen Volcano (Kamchatka): Insights into magma-chamber processes
Author:
Publisher
Pleiades Publishing Ltd
Subject
Metals and Alloys,Geophysics,Geotechnical Engineering and Engineering Geology
Link
http://link.springer.com/content/pdf/10.1134/S0742046313020024.pdf
Reference44 articles.
1. Allègre, C.J., Provost, A., and Jaupart, C., Oscillatory zoning: a pathological case of crystal growth, Nature, 1981, vol. 294, pp. 223–228.
2. Ariskin, A.A., Barmina, G.S., Frenkel, M.Ya., and Nielsen, R.L., COMAGMAT: a Fortran program to model magma differentiation processes, Comput. Geosci., 1993, vol. 19, pp. 1155–1170.
3. Bindeman, I.N., Davis, A.M., and Drake, M.J., Ion microprobe study of plagioclase-basalt partition experiments at natural concentration level of trace elements, Geochim. Cosmochim. Acta, 1998, vol. 62, no. 7, p. 1175.
4. Brophy, J.G., Dorais, M.J., Donnelly-Nolan, J., and Singer, B.S., A textural and compositional (ion-probe and electron probe) study of plagioclase zonation styles in hornblende gabbro cumulates from Little Glass Mountain, Medicine Lake Volcano, California: implications for fractional crystallization mechanisms in calc-alkaline magma genesis, Contrib. Mineral. Petrol., 1996, vol. 126, p. 121–136.
5. Browne, B.L., Eichelberger, J.C., Patino, L.C., et al., Magma mingling as indicated by texture and Sr/Ba ratios of plagioclase phenocrysts from Unzen Volcano, SW Japan, J. Volcanol. Geothermal Res., 2006, vol. 154, pp. 103–116.
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