Browsing by Author "Veksler I.V."
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Browsing by Author "Veksler I.V."
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Veksler I.V.; Thomas R. (2002)Extreme enrichment in H2O, B, P and F is characteristic of many evolved granites and pegmatites. We report experimental phase relations of a synthetic peraluminous pegmatite spiked with P2O5, B2O3 and F (5 wt% of each), ...
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Veksler I.V.; Dorfman A.M.; Dingwell D.B.; Zotov N. (2002)The main objectives of this study were to investigate conditions for stable and metastable liquid immiscibility in dry borosilicate synthetic systems and to evaluate effects of temperature and bulk melt composition on ...
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Badanina E.V.; Thomas R.; Veksler I.V.; Trumbull R.B.; Syritso L.F. (2003)Boron is a typical lithophile element characterized by a significant accumulation in the Earth's crust (15 ppm) relative to the primitive mantle (0.6 ppm) [1]. In magmatic systems, boron behaves as an incompatible element ...
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Veksler I.V. (2004)Several types of fluid immiscibility may affect the evolution of volatile-rich magmatic systems at the magmatic–hydrothermal transition. The topology of silicate–salt–H2O systems implies that three-fluid immiscibility ...
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Badanina E.V.; Veksler I.V.; Thomas R.; Trumbull R.B.; Syritso L.F. (2004)We report compositions of homogenized quartz-hosted melt inclusions from a layered sequence of Li-, F-rich granites in the Khangilay complex that document the range of melt evolution from barren biotite granites to Ta-rich, ...
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Veksler I.V.; Nielsen T.F.D.; Sokolov S.V. (1998)Cumulus olivine, clinopyroxene, melilite and perovskite from silicate rocks and carbonatites of the Gardiner (East Greenland) and Kovdor (Kola Peninsula) ultramafic alkaline complexes contain primary melt inclusions ...
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Veksler I.V.; Keppler H. (2000)Experimental studies of the element distribution between carbonatite melts and hydrous fluids are hampered by the fact that neither the fluid nor the melt can be isochemically quenched in conventional high-pressure vessels. ...
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Veksler I.V.; Teptelev M.P. (1989)The mineralogy and geochemistry of titanium in rocks of the ultramafic-alkalic association are complex and varied. The reasons are, first, the high concentration of titanium in the primary magmas of this association, and, ...
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Veksler I.V.; Fedorchuk Y.M.; Nielsen T.F.D. (1998)The evolution of nephelinitic melts in equilibrium with mica-bearing liquidus assemblages and melting relations have been studied on two silica-undersaturated joins of the KAlSiO4- Mg2SiO4- Ca2SiO4- SiO2- F system at ...
Now showing items 1-9 of 9