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Kozai, Y. (2005) Experimental study on diamond dissolution in kimberlitic and lamproitic melts at 1300-1420  C and 1 GPa with controlled oxygen partial pressure. American Mineralogist, 90 (11) 1759-1766 doi:10.2138/am.2005.1862

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Reference TypeJournal (article/letter/editorial)
TitleExperimental study on diamond dissolution in kimberlitic and lamproitic melts at 1300-1420  C and 1 GPa with controlled oxygen partial pressure
JournalAmerican Mineralogist
AuthorsKozai, Y.Author
Year2005 (November 1)Volume90
Page(s)1759-1766Issue11
PublisherMineralogical Society of America
DOIdoi:10.2138/am.2005.1862Search in ResearchGate
Mindat Ref. ID395201Long-form Identifiermindat:1:5:395201:0
GUID41b60357-80d5-4425-a481-fdebcdc16853
Full ReferenceKozai, Y. (2005) Experimental study on diamond dissolution in kimberlitic and lamproitic melts at 1300-1420  C and 1 GPa with controlled oxygen partial pressure. American Mineralogist, 90 (11) 1759-1766 doi:10.2138/am.2005.1862
Plain TextKozai, Y. (2005) Experimental study on diamond dissolution in kimberlitic and lamproitic melts at 1300-1420  C and 1 GPa with controlled oxygen partial pressure. American Mineralogist, 90 (11) 1759-1766 doi:10.2138/am.2005.1862
In(2005, November) American Mineralogist Vol. 90 (11) Mineralogical Society of America

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Santillan, J. (2005) An infrared study of carbon-oxygen bonding in magnesite to 60 GPa. American Mineralogist, 90 (10) 1669-1673 doi:10.2138/am.2005.1703
Khokhryakov, A. F., Pal'yanov, Y. N. (2010) Influence of the fluid composition on diamond dissolution forms in carbonate melts. American Mineralogist, 95 (10) 1508-1514 doi:10.2138/am.2010.3451
Ono, S. (2005) Post-aragonite phase transformation in CaCO3 at 40 GPa. American Mineralogist, 90 (4) 667-671 doi:10.2138/am.2005.1610
Winther, K. Tobias, Watson, E. Bruce, Korenowski, Gerald M. (1998) Magmatic sulfur compounds and sulfur diffusion in albite melt at 1 GPa and 1300-1500 degrees C. American Mineralogist, 83 (11) 1141-1151 doi:10.2138/am-1998-11-1201
Hu, X. (2005) Growth and dissolution kinetics at the dolomite-water interface: An in-situ scanning probe microscopy study. American Mineralogist, 90 (5) 963-968 doi:10.2138/am.2005.1798
Nakatsuka, A. (2005) Crystal structure of single-crystal CaGeO3 tetragonal garnet synthesized at 3 GPa and 1000  C. American Mineralogist, 90 (4) 755-757 doi:10.2138/am.2005.1801
Tarantino, S. C. (2005) Mixing and ordering behavior in manganocolumbite-ferrocolumbite solid solution: A single-crystal X-ray diffraction study. American Mineralogist, 90 (8) 1291-1300 doi:10.2138/am.2005.1641
Colasanti, C. V., Johnson, E. A., Manning, C. E. (2011) An experimental study of OH solubility in rutile at 500-900  C, 0.5-2 GPa, and a range of oxygen fugacities. American Mineralogist, 96 (8) 1291-1299 doi:10.2138/am.2011.3708
Arima, Makoto, Kozai, Yusuke (2008) Diamond dissolution rates in kimberlitic melts at 13001500 C in the graphite stability field. European Journal of Mineralogy, 20 (3) 357-364 doi:10.1127/0935-1221/2008/0020-1820
Allwardt, J. R. (2005) The effect of fictive temperature on Al coordination in high-pressure (10 GPa) sodium aluminosilicate glasses. American Mineralogist, 90 (8) 1453-1457 doi:10.2138/am.2005.1736
Luttge, A. (2005) Etch pit coalescence, surface area, and overall mineral dissolution rates. American Mineralogist, 90 (11) 1776-1783 doi:10.2138/am.2005.1734
 
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