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Ilya V. Veksler

Researcher at University of Potsdam

Publications -  61
Citations -  2979

Ilya V. Veksler is an academic researcher from University of Potsdam. The author has contributed to research in topics: Melt inclusions & Silicate. The author has an hindex of 25, co-authored 58 publications receiving 2557 citations. Previous affiliations of Ilya V. Veksler include Technical University of Berlin & University of Bayreuth.

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Trace Element Partitioning in Immiscible Silicate–Carbonate Liquid Systems: an Initial Experimental Study Using a Centrifuge Autoclave

TL;DR: The origin of carbonatites remains a contentious topic as discussed by the authors and the role of liquid immiscibility between silicate and carbonate liquids has been often been carbonate liquid has often been proposed.
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Liquid immiscibility and its role at the magmatic–hydrothermal transition: a summary of experimental studies

Ilya V. Veksler
- 27 Oct 2004 - 
TL;DR: In this article, the Coulombic properties (electric charges Z and ionic radii r) of the main network-modifying cations and the capacity for immiscibility appears to decrease in the following sequence: Mg>Ca>Sr>Ba>Li>Na>K.
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Immiscible iron- and silica-rich melts in basalt petrogenesis documented in the Skaergaard intrusion

TL;DR: The first finding of immiscible iron and silica-rich melts in a plutonic environment documented in the Skaergaard intrusion, East Greenland is reported in this article.
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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

TL;DR: In this article, the tetrad effect was demonstrated in the partitioning of rare earth elements between immiscible silicate and fluoride melts, and the decoupling of Y and Ho was demonstrated.
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Partitioning of elements between silicate melt and immiscible fluoride, chloride, carbonate, phosphate and sulfate melts, with implications to the origin of natrocarbonatite

TL;DR: In this paper, liquid-liquid partitioning of 42 elements between synthetic silicate melts and immiscible fluoride, chloride, carbonate, phosphate and sulfate liquids was studied at temperatures of 650-1100°C, pressures 72-100MPa, with 0 −11.% H2O.