Inhaltsbereich
Publications
(Co) Author: Dobrzhinetskaya, L.
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(2013): First find of polycrystalline diamond in ultrahigh-pressure metamorphic terrane of Erzgebirge, Germany. Journal of Metamorphic Geology, 31, 1, 5-18.| EDOC: 19381 | 10.1111/jmg.12010 |
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(2010): Nanosims studies of ∂ 15N and ∂ 13C in nitrides inclusions in coesite from a Tibetan massive cromitite ore. Geochimica et Cosmochimica Acta, 74, 12, Suppl. 1, 680.| EDOC: 15295 |
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(2009): Phlogopite and quartz lamellae in diamond-bearing diopside from marbles of the Kokchetav massif, Kazakhstan: exsolution or replacement reaction?. Journal of Metamorphic Geology, 27, 9, 607-620.
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(2009): High-pressure highly reduced nitrides and oxides from chromitite of a Tibetan ophiolite. Proceedings of the National Academy of Sciences of the United States of America (PNAS), 106, 46, 19233-19238.
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(2009): Lamellae of phyllosilicates in K-rich diopside from UHP marble of the Kokchetav massiv, Kazakhstan: FIB-TEM and synchrotron IR studies. Geochimica et Cosmochimica Acta, 73, 13, Suppl. 1, A296.| EDOC: 13283 |
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(2008): Fluids role in formation of microdiamonds from ultrahigh pressure metamorphic terranes. Geochimica et Cosmochimica Acta, 72, 12, Suppl. 1, A221.| EDOC: 12640 |
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(2008): Boron and Nitrogen in ultrahigh-pressure terrestrial rocks. Geochimica et Cosmochimica Acta, 72, 12, Suppl. 1, A221.| EDOC: 12643 |
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(2007): A look inside of diamond-forming media in deep subduction zones. Proceedings of the National Academy of Sciences of the United States of America (PNAS), 104, 22, 9128-9132.
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(2007): Diamond- and coesite-bearing chromitites from the Luobusa ophiolite, Tibet. Geology, 35, 10, 875-878.| EDOC: 10257 | 10.1130/G23766A.1 |
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(2006): Nanometric inclusions of Carbonates in Kokchetav diamonds from Kazakhstan; a new constraint for the depth of metamorphic diamond crystallization. Earth and Planetary Science Letters, 243, 1-2, 85-93.
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(2005): Direct observation and analysis of a trapped COH fluid growth medium in metamorphic diamond. Terra Nova, 17, 5, 472-477.
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(2001): Electron microscope study of the reaction olivine +H2O +TiO2 --> titanoclinohumite + titanochondrodite synthesized at 8 GPa, 1300 K. American Mineralogist, 86, 5-6, 601-610.| EDOC: 301 |
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