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Name: Lizardite RRUFF ID: R060006 Ideal Chemistry: Mg3Si2O5(OH)4 Locality: Snarum, Norway Source: University of Arizona Mineral Museum 2896 Owner: RRUFF Description: Green blebs of fine-grained serpentine habit, polytype 1T, associated with pearly hydrotalcite Status: The identification of this mineral has been confirmed by X-ray diffraction and chemical analysis |
Mineral Groups: [ serpentine (12) ] [ Clay (86) ] |
CHEMISTRY | ||||||||||
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RAMAN SPECTRUM | ||||||||||||
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BROAD SCAN WITH SPECTRAL ARTIFACTS | ||||||||||||
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INFRARED SPECTRUM (Attenuated Total Reflectance) | |||||||||||||||
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POWDER DIFFRACTION | ||||||||
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RRUFF ID: | R060006.1 | |||||||
Sample Description: | Powder | |||||||
Cell Refinement Output: |
a: 5.3258(7)Å b: 5.3258(7)Å c: 7.273(2)Å alpha: 90° beta: 90° gamma: 120° Volume: 178.67(6)Å3 Crystal System: hexagonal |
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REFERENCES for Lizardite | |
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American Mineralogist Crystal Structure Database Record: [view record] |
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Anthony J W, Bideaux R A, Bladh K W, and Nichols M C (1990) Handbook of Mineralogy, Mineral Data Publishing, Tucson Arizona, USA, by permission of the Mineralogical Society of America. [view file] |
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Whittaker E J W, Zussman J (1956) The characterization of serpentine minerals by X-ray diffraction, Mineralogical Magazine, 31, 107-126 [view file] |
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Fleischer M (1957) New mineral names, American Mineralogist, 42, 580-586 [view file] |
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Zussman J, Brindley G W, Comer J J (1957) Electron diffraction studies of serpentine minerals, American Mineralogist, 42, 133-153 [view file] |
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Krstanovic I (1968) Crystal structure of single layer lizardite, Zeitschrift für Kristallographie, 126, 163-169 [view file] |
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Brindley G W, Wan H-M (1975) Compositions, structures, and thermal behavior of nickel-containing minerals in the lizardite-nepouite series, American Mineralogist, 60, 863-871 [view file] |
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Bish D L, Brindley G W (1978) Deweylites, mixtures of poorly crystalline hydrous serpentine and talc-like minerals, Mineralogical Magazine, 42, 75-84 [view file] |
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Caruso L J, Chernosky J V (1979) The stability of lizardite, The Canadian Mineralogist, 17, 757-769 [view file] |
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Veblen D R, Buseck P R (1979) Serpentine minerals: Intergrowth and new combination structures, Science, 206, 1398-1400 [view file] |
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Wicks F J (1986) Lizardite and its parent enstatite: a study by X-ray diffraction and transmission electron microscopy, The Canadian Mineralogist, 24, 775-788 [view file] |
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Mellini M, Zanazzi P F (1989) Effects of pressure on the structure of lizardite-1T, European Journal of Mineralogy, 1, 13-19 |
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O'Hanley D S, Chernosky J V, Wicks F J (1989) The stability of lizardite and chrysotile, The Canadian Mineralogist, 27, 483-493 [view file] |
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Wicks F J, Kjoller K, Henderson G S (1992) Imaging the hydroxyl surface of lizardite at atomic resolution with the atomic force microscope, The Canadian Mineralogist, 30, 83-91 [view file] |
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Krstanovic I, Karanovic L (1995) Crystal structure of two lizardites, Mg3Si2O5(OH)4, Neues Jahrbuch für Mineralogie, Monatshefte, 1995, 193-201 |
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O'Hanley D S, Wicks F J (1995) Conditions of formation of lizardite, chrysotile and antigorite, Cassiar, British Columbia, The Canadian Mineralogist, 33, 753-773 [view file] |
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Bard D, Yarwood J, Tylee B (1997) Asbestos fibre identification by Raman microspectroscopy, Journal of Raman Spectroscopy, 28, 803-809 [link] |
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O'Hanley D S, Dyar M D (1998) The composition of chrysotile and its relationship with lizardite, The Canadian Mineralogist, 36, 727-798 [view file] |
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Rinaudo C, Gastaldi D, Belluso E (2003) Characterization of chrysotile, antigorite and lizardite by FT-Raman spectroscopy, The Canadian Mineralogist, 41, 883-890 [view file] |
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Evans B W (2004) The serpentinite multisystem revisited: chrysotile is metastable, International Geology Review, 46, 479-506 |
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Hamilton V E, McSween H Y, Hapke B (2005) Mineralogy of Martian atmospheric dust inferred from thermal infrared spectra of aerosols, Journal of Geophysical Research, 110, E12006 [link] |
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Wicks F J, Chatfield E J (2005) Scrolling of thin crystals of lizardite: an expression of internal stress, The Canadian Mineralogist, 43, 1993-2004 [view file] |
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Auzende A L, Pellenq R J M, Devouard B, Baronnet A, Grauby O (2006) Atomistic calculations of structural and elastic properties of serpentine minerals: the case of lizardite, Physics and Chemistry of Minerals, 33, 266-275 |
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Prencipe M, Noel Y, Bruno M, Dovesi R (2009) The vibrational spectrum of lizardite-1T [Mg3Si2O5(OH)4] at the Γ point: A contribution from an ab initio periodic B3LYP calculation, American Mineralogist, 94, 986-994 [view file] |
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Laurora A, Brigatti M F, Malferrari D, Galli E, Rossi A, Ferrari M (2011) The crystal chemistry of lizardite-1T from northern Apennines ophiolites near Modena, Italy, The Canadian Mineralogist, 49, 1045-1054 [view file] |
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Trittschack R, Grobéty B, Koch-Müller M (2012) In situ high-temperature Raman and FTIR spectroscopy of the phase transformation of lizardite, American Mineralogist, 97, 1965-1976 [view file] |
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Tsuchiya J (2013) A first-principles calculation of the elastic and vibrational anomalies of lizardite under pressure, American Mineralogist, 98, 2046-2052 |
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Wicks F J, Dunn P J, Back M E, Ramik R A (2015) "Maufite" discredited: Not a mineral species but an important interstratified Ni-bearing lizardite + clinochlore, The Canadian Mineralogist, 53, 911-920 [view file] |
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Baron F, Petit S (2016) Interpretation of the infrared spectra of the lizardite-nepouite series in the near- and mid-infrared range, American Mineralogist, 101, 423-430 |
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