21 results on '"Aranovich, L. Y."'
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2. Clorine Solubility in Silicate Melts: New Experiments and Thermodynamic Mixing Model
3. Interaction of Fe3C with Hydrogen: On the Compatibility of Carbon with Hydrogen in Metallic Iron
4. Equations of State for NaCl and CaCl2 Solutions of Arbitrary Concentration at Temperatures 423.15–623.15 K and Pressures up to 5 kbar
5. An Empirical Model of the Gibbs Free Energy for Solutions of NaCl and CaCl2 of Arbitrary Concentration at Temperatures from 423.15 K to 623.15 K under Vapor Saturation Pressure
6. Morphology and impurity elements of zircon in the oceanic lithosphere at the Mid-Atlantic ridge axial zone (6°–13° N): Evidence of specifics of magmatic crystallization and postmagmatic transformations
7. Isotope Characteristics of Carbonates from Rocks of Greenstone Belts as an Indicator of a Possible Source of Fluids in Precambrian Granulite Complexes: An Example from the Giyani Greenstone Belt and the Limpopo Granulite Complex, South Africa
8. Interaction of Fe3C with Hydrogen: On the Compatibility of Carbon with Hydrogen in Metallic Iron.
9. H2O activity in concentrated KCl and KCl-NaCl solutions at high temperatures and pressures measured by the brucite-periclase equilibrium
10. Optimized standard state and solution properties of minerals: II. Comparisons, predictions, and applications
11. Optimized standard state and solution properties of minerals: I. Model calibration for olivine, orthopyroxene, cordierite, garnet, and ilmenite in the system FeO-MgO-CaO-Al2O3-TiO2-SiO2
12. H2O activity in concentrated NaCl solutions at high pressures and temperatures measured by the brucite-periclase equilibrium
13. Reassessment of the garnet-clinopyroxene Fe−Mg exchange thermometer: I. Evaluation of the Pattison and Newton (1989) experiments
14. Equations of State for NaCl and CaCl2 Solutions of Arbitrary Concentration at Temperatures 423.15-623.15 K and Pressures up to 5 kbar.
15. An Empirical Model of the Gibbs Free Energy for Solutions of NaCl and CaCl2 of Arbitrary Concentration at Temperatures from 423.15 K to 623.15 K under Vapor Saturation Pressure.
16. Reversed phase equilibrium constraints on the stability of Mg-Fe-Al biotite
17. The Problem of Depth in Geology: When Pressure Does Not Translate into Depth
18. Experimental determination of CO2-H2O activity-composition relations at 600-1000 degrees C and 6-14 kbar by reversed decarbonation and dehydration reactions
19. H 2 O activity in concentrated KCl and KCl-NaCl solutions at high temperatures and pressures measured by the brucite-periclase equilibrium
20. H 2 O activity in concentrated NaCl solutions at high pressures and temperatures measured by the brucite-periclase equilibrium
21. Reassessment of the garnet-clinopyroxene Fe-Mg exchange thermometer: I. Evaluation of the Pattison and Newton (1989) experiments
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