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Capitani, G. C., Stixrude, L. (2012) A first-principle investigation of antigorite up to 30 GPa: Structural behavior under compression. American Mineralogist, 97 (7) 1177-1186 doi:10.2138/am.2012.3956

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Reference TypeJournal (article/letter/editorial)
TitleA first-principle investigation of antigorite up to 30 GPa: Structural behavior under compression
JournalAmerican Mineralogist
AuthorsCapitani, G. C.Author
Stixrude, L.Author
Year2012 (July 1)Volume97
Issue7
PublisherMineralogical Society of America
DOIdoi:10.2138/am.2012.3956Search in ResearchGate
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Mindat Ref. ID397011Long-form Identifiermindat:1:5:397011:3
GUID0
Full ReferenceCapitani, G. C., Stixrude, L. (2012) A first-principle investigation of antigorite up to 30 GPa: Structural behavior under compression. American Mineralogist, 97 (7) 1177-1186 doi:10.2138/am.2012.3956
Plain TextCapitani, G. C., Stixrude, L. (2012) A first-principle investigation of antigorite up to 30 GPa: Structural behavior under compression. American Mineralogist, 97 (7) 1177-1186 doi:10.2138/am.2012.3956
In(2012, July) American Mineralogist Vol. 97 (7) Mineralogical Society of America

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Capitani, G. C., Stixrude, L., Mellini, M. (2009) First-principles energetics and structural relaxation of antigorite. American Mineralogist, 94 (8) 1271-1278 doi:10.2138/am.2009.3218
Capitani, G. C., Mellini, M. (2007) High-resolution transmission electron microscopy (HRTEM) investigation of antigorite polysomes (m = 15 to 18) American Mineralogist, 92 (1) 64-71 doi:10.2138/am.2007.2188
Ullrich, A., Miletich, R., Nestola, F., Weikusat, C., Ohashi, H. (2009) Lattice compression and structural behavior of NaVSi2O6 clinopyroxene to 11 GPa. American Mineralogist, 94 (4) 557-564 doi:10.2138/am.2009.2993
Capitani, G. C., Mellini, M. (2008) Rationale for the existence of four- and eight-reversals in antigorite. American Mineralogist, 93 (5) 796-799 doi:10.2138/am.2008.2538
Capitani, G. C. (2006) The crystal structure of a second antigorite polysome (m = 16), by single-crystal synchrotron diffraction. American Mineralogist, 91 (2) 394-399 doi:10.2138/am.2006.1919
Capitani, G. (2005) HRTEM evidence for 8-reversals in the m = 17 antigorite polysome. American Mineralogist, 90 (5) 991-999 doi:10.2138/am.2005.1634
Williams, Q., Knittle, E., Scott, H. P., Liu, Z. (2012) The high-pressure behavior of micas: Vibrational spectra of muscovite, biotite, and phlogopite to 30 GPa. American Mineralogist, 97 (1) 241-252 doi:10.2138/am.2012.3824
Yamanaka, T., Uchida, A., Nakamoto, Y. (2008) Structural transition of post-spinel phases CaMn2O4, CaFe2O4, and CaTi2O4 under high pressures up to 80 GPa. American Mineralogist, 93 (11) 1874-1881 doi:10.2138/am.2008.2934
Greaux, S., Gautron, L., Andrault, D., Bolfan-Casanova, N., Guignot, N., Haines, J. (2008) Structural characterization of natural UO2 at pressures up to 82 GPa and temperatures up to 2200 K. American Mineralogist, 93 (7) 1090-1098 doi:10.2138/am.2008.2735
Wentzcovitch, Renata M., Stixrude, Lars (1997) Crystal chemistry of forsterite; a first-principles study. American Mineralogist, 82 (7) 663-671 doi:10.2138/am-1997-7-802
Eggler, D. H., Ehmann, A. N. (2010) Rate of antigorite dehydration at 2 GPa applied to subduction zones. American Mineralogist, 95 (5) 761-769 doi:10.2138/am.2010.3227
 
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