Inhaltsbereich
Publications
(Co) Author: Khisina, N. R.
| Paper (ISI journals) [11] |
Paper (further journals) [4] |
Chapter in Book [1] |
Conference Paper [12] |
All [28] |
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(2013): Oriented chromite-diopside symplectic inclusions in olivine from lunar regolith delivered by. Geochimica et Cosmochimica Acta, 104, 84-98.
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(2011): Chemical and Phase Heterogeneity of Ti-Fe-Mn-Silica Microspherules in Crushed Ore Samples. Geochemistry International, 49, 11, 1111-1119.
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(2011): Lamellar Pyroxene-Spinel Symplectites in Lunar Olivine from the Luna 24 Regolith. Geochemistry International, 49, 5, 449-458.
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(2010): The behavior of protons during wet olivine deformation under the conditions of the kimberlite process. Geokhimiya, 48, 4, 357-365.
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(2008): Nanoinclusions of High-Pressure Hydrous Silicate, Mg3Si4O10(OH)2 . nH2O (10Å-Phase), in Mantle Olivine: Mechanisms of Formation and Transformation. Geochemistry International, 46, 4, 319-327.
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(2003): First principle study of (MgH2SiO4).n(Mg2SiO4) hydrous olivine structures. I. Crystal structure modeling of hydrous olivine Hy-2a(MgH2SiO4).3(Mg2SiO4). Physics and Chemistry of Minerals, 30, 1, 1-11.| EDOC: 3427 |
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(2002): Hydrous olivine (Mg1-yFe2+y)2-xvxSiO4H2x - a new DHMS phase of variable composition observed as nanometer sized precipitations in mantle olivine. Physics and Chemistry of Minerals, 29, 2, 98-111.| EDOC: 2937 |
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(2002): Modes of OH-occurrence in mantle olivine. I. Structural hydroxyl. Geochemistry International, 40, 4, 332-341.| EDOC: 8217 |
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(2001): Microstructure of experimentally oxidized olivine from a mantle nodule: II. Phase composition of crystalline microinclusions containing Fe3+ and OH-. Geochemistry International, 39, 7, 655-666.| EDOC: 2775 |
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(2001): Extrinsic and Intrinsic mode of hydrogen occurrence in natural olivines: FTIR and TEM investigation. Physics and Chemistry of Minerals, 28, 5, 291-301.
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(2000): Nano-scale microstructure of Fe3+-, OH-bearing crystalline inclusions in experimentally oxidized olivine from a mantle nodule. Mineralogical Magazine, 64, 2, 319-335.| EDOC: 336 |
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