Inhaltsbereich
Publications
(Co) Author: Green, H. W.
| Paper (ISI journals) [8] |
Conference Paper [11] |
All [19] |
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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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(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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(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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(2012): Experiments on Graphitization of Diamond in the Presence of Water: Implications for Exhumation of Ultrahigh Pressure Metamorphic Rocks. AGU 2012 Fall Meeting (San Francisco, USA 2012).| EDOC: 20684 |
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(2011): Fluids Speciation in Deep Subduction Channels: Evidence From Polycrystalline Diamonds From UHPM Terranes. AGU 2011 Fall Meeting (San Francisco, USA 2011).| EDOC: 18013 |
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(2010): Tubular Mg-ferrite in magnesiowüstite inclusions in diamond from superdeep origin: control of Fe-valence by dislocation core structure. IMA 2010 - 20th General Meeting of the International Mineralogical Association (Budapest, Hungary 2010), 210.| EDOC: 15474 |
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(2009): New geological settings for ultra-high pressure rocks. AGU 2009 Joint Assembly (Toronto, Canada 2009), V04.| EDOC: 13767 |
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(2009): Tubular Mg-ferrite in Mg-wüstite inclusions in diamond of superdeep origin: control of Fe-valence by crystallographic structure. AGU 2009 Fall Meeting (San Francisco 2009), V54B-07.| EDOC: 14250 |
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(2007): Unusal mineral assemblage of titanium and boron nitrides in podiform chromitite of Tibet: are they from Earth's deep interior?. Frontiers in Mineral Sciences 2007 (Cambridge, UK 2007), 189.| EDOC: 9937 |
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(2006): Diamond and coesite after former stishovite in Tibet ophiolites: Is that myth or reality?. AGU Fall Meeting (San Francisco, USA 2006).| EDOC: 9428 |
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(2005): Inclusions in diamonds from UHPM terranes: a new constraint for depth of subduction and exhumation. 7th International Eclogite Conference (Seggau, Austria 2005), 32.| EDOC: 7459 |
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(2004): Nanometric inclusions in diamonds: a new constraint for the origin of diamonds in orogenetic belts. 32nd International Geological Congress (Florence, Italy 2004).| EDOC: 6036 |
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(2000): Experimental synthesis of Ti-clinohumite in fluorine-free systems at 8-10 GPa and T=1300-1500K. AGU 2000 Fall Meeting (San Francisco 2000).| EDOC: 2115 |
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(1999): Electron Microscope Studies of the Reaction Olivine -> Ti-clinohumite + Ti-chondrodite synthesized at 8 GPa, 1300 K. AGU 1999 Fall Meeting (San Francisco 1999), 928.| EDOC: 2254 |