Inhaltsbereich
Scientific Drilling ICDP Publications
(Co) Author: Veksler, I. V.
(since 2002) [ All ]
| Paper (ISI journals) [28] |
Paper (further journals) [2] |
Chapter in Book [3] |
Conference Paper [34] |
All [67] |
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(2012): Partitioning of elements between silicate melt and immiscible fluoride, chloride, carbonate, phosphate and sulfate melts, with implications to the origin of natrocarbonatite. Geochimica et Cosmochimica Acta, 79, 15, 20-40.
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(2011): Silicate Liquid Immiscibility within the Crystal Mush: Late-stage Magmatic Microstructures in the Skaergaard Intrusion, East Greenland. Journal of Petrology, 52, 1, 175-222.
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(2011): Crystallization of the Skaergaard Intrusion from an Emulsion of Immiscible Iron- and Silica-rich Liquids: Evidence from Melt Inclusions in Plagioclase. Journal of Petrology, 52, 2, 345-373.
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(2011): On the significance of ultra-magnesian olivines in basaltic rocks. Mineralogical Magazine, 75, 3, 1164.| EDOC: 17420 |
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(2011): On the significance of ultra-magnesian olivines in basaltic rocks. Geology, 39, 12, 1095-1098.| EDOC: 17715 | 10.1130/G32214.1 |
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(2011): F, Cl and S contents of olivine-hosted melt inclusions from picritic dike rocks, Etendeka, NW Namibia. Mineralogical Magazine, 75, 3, 2177.| EDOC: 17421 |
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(2010): Interfacial tension between immiscible liquids in alkaline earth - boron oxide binary systems. Journal of Non-Crystalline Solids, 356, 23-24, 1163-1167.
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(2010): Interfacial tension between immiscible liquids in the system K2O-FeO-Fe2O3-Al2O3-SiO2 and implications for the kinetics of silicate melt unmixing. American Mineralogist, 95, 11-12, 1679-1685.
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(2009): Extreme iron enrichment and liquid immiscibility in mafic intrusions: experimental evidence revisited. Lithos, 111, 72-82.
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(2008): Liquid immiscibility and evolution of basaltic magma: reply to S. A. Morse, A. R. McBirney and A. R. Philpotts. Journal of Petrology, 49, 12, 2177-2186.
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(2008): Liquid unmixing kinetics and the extent of immiscibility in the system K2O-CaO-FeO-Al2O3-SiO2. Chemical Geology, 256, 3-4.
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(2007): Liquid Immiscibility and the Evolution of Basaltic Magma. Journal of Petrology, 48, 11, 2187-2210.
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(2007): Kinetics of liquid immiscibility in the system K2O-CaO-FeO-Al2O3-SiO2. Geochimica et Cosmochimica Acta, 71, 15, Suppl. 1, A1061.| EDOC: 10120 |
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(2006): The behavior of rare-earth and lithophile trace elements in rara-metal granites: A study of fluorite, melt inclusions and host rocks from the Khangilay complex, Transbaikalia, Russia.. Canadian Mineralogist, 44, 3, 667-692.| EDOC: 8996 |
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(2006): Immiscible silicate liquid partition coefficients; implications for crystal-melt element partitioning and basalt petrogenesis. Contributions to Mineralogy and Petrology, 152, 6, 685-702.
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(2005): Matrix effect and partitioning of boron isotopes between immiscible Si-rich and B-rich liquids in the Si–Al–B–Ca–Na–O system: A SIMS study of glasses quenched from centrifuge experiments. Chemical Geology, 222, 3-4, 268-280.
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(2005): Immiscible iron- and silica-rich melts in basalt petrogenesis documented in the Skaergaard intrusion. Geology, 33, 11, 885-888.| EDOC: 8300 | 10.1130/G21724.1 |
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(2005): Partitioning of lanthanides and Y between immiscible silicate and fluoride melts, fluorite and cryolite and the origin of the lanthanide tetrad effect in igneous rocks. Geochimica et Cosmochimica Acta, 69, 11, 2847-2860.
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(2004): Magmatic evolution of Li-F, rare-metal granites: a case study of melt inclusions in the Khangilay complex, Eastern Transbaikalia (Russia). Chemical Geology, 210, 1-4, 113-133.
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(2004): Liquid immiscibility and its role at the magmatic-hydrothermal transition: a summary of experimental studies. Chemical Geology, 210, 1-4, 7-31.
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(2003): High boron concentration in a Li-F granitic melt. Doklady Earth Sciences, 390, 4, 529-532.| EDOC: 5676 |
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(2003): Crystallization of AlpO4-SiO2 solid solutions from granitic melt and implications for P-rich melt inclusions in pegmatitic quartz. American Mineralogist, 88, 11-12, Pt.1, 1724-1730.| EDOC: 5678 |
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(2003): Crystallization of AlPO4-SiO2 solid solutions from granitic melt and implications to P-rich melt inclusions in pegmatitic quartz. American Mineralogist, 88, 11-12, Pt. 1, 1724-1730.| EDOC: 4205 |
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(2002): Is natrocarbonatite a cognate fluid condensate?. Contributions to Mineralogy and Petrology, 142, 4, 425-435.| EDOC: 2883 |
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(2002): Element partitioning between immiscible borosilicate liquids: a high-temperature centrifuge study. Geochimica et Cosmochimica Acta, 66, 14, 2603-2614.| EDOC: 2887 |
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(2002): An experimental study of B-, P- and F-rich synthetic granite pegmatite at 0.1 and 0.2 GPa. Contributions to Mineralogy and Petrology, 143, 6, 673-683.| EDOC: 2914 |
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(2002): Experimental evidence of three coexisting immiscible fluids in synthetic granite pegmatite. American Mineralogist, 87, 5-6, 775-779.| EDOC: 2859 |
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(2002): Experimental evidence of three coexisting immiscible fluids in synthetic granitic pegmatite. American Mineralogist, 87, 775-779.| EDOC: 3288 |


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