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Mineral contains: Grunerite   

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Apopei A I, Buzgar N (2010) The Raman study of amphiboles. Analele Stiintifice Ale Universitatii, Al. I. Cuza Iasi Geologie 56, 57-83

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Bard D, Yarwood J, Tylee B (1997) Asbestos fibre identification by Raman microspectroscopy. Journal of Raman Spectroscopy 28, 803-809

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Boffa Ballaran T, Carpenter M A (2003) Line broadening and enthalpy: Some empirical calibrations of solid solution behaviour from IR spectra. Phase Transitions 76, 137-154

Finger L W (1969) The crystal structure and cation distribution of a grunerite. Mineralogical Society of America Special Paper 2, 95-100

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Germine M, Puffer J H (2020) Analytical transmission electron microscopy of amosite asbestos from South Africa. Archives of Environmental & Occupational Health 75, 36-44

Goldman D S, Rossman G R (1982) The identification of Fe2+ in the M4 site of calcic amphiboles: reply. American Mineralogist 67, 340-342

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Gunter M E (2010) Defining asbestos: differences between the built and natural environments. Chimia 64, 747-752

Harper M, Lee E G, Doorn S S, Hammond O (2008) Differentiating non-asbestiform amphibole and amphibole asbestos by size characteristics. Journal of Occupational and Environmental Hygiene 5, 761-770

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Hirschmann M, Evans B W, Yang H (1994) Composition and temperature dependence of Fe-Mg ordering in cummingtonite-grunerite as determined by X-ray diffraction. American Mineralogist 79, 862-877

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Huang E P (2002) Raman spectroscopic study of amphiboles. Doctoral Dissertation 1, 1-138

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Kenngott A (1853) VIII. Ordnung: Spathe. IX. Geschlecht: Augit-Spathe. 4. Grunerit. in Das Mohs'sche Mineralsystem, Verlag und Druck (Wien) 62-77

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Klein C (1964) Cummingtonite-grunerite series: A chemical, optical and x-ray study. American Mineralogist 49, 963-982

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Leake B E (1978) Nomenclature of amphiboles. American Mineralogist 63, 1023-1052

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Leake B E, Woolley A R, Arps C E S, Birch W D, Gilbert M C, Grice J D, Hawthorne F C, Kato A, Kisch H J, Krivovichev V G, Linthout K, Laird J, Mandarino J A, Maresch W V, Nickel E H, Rock N M S, Schumacher J C, Smith D C, Stephenson N C N, Ungaretti L, Whittaker E J W, Youzhi G (1997) Nomenclature of amphiboles: report of the Subcommittee on Amphiboles of the International Mineralogical Association, Commission on New Minerals and Mineral Names. The Canadian Mineralogist 35, 219-246

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Leake B E, Woolley A R, Birch W D, Burke E A J, Ferraris G, Grice J D, Hawthorne F C, Kisch H J, Krivovichev V G, Schumacher J C, Stephenson N C N, Whittaker E J W (2003) Nomenclature of amphiboles: additions and revisions to the International Mineralogical Association’s 1997 recommendations. The Canadian Mineralogist 41, 1355-1362

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Rinaudo C, Belluso E, Gastaldi D (2004) Assessment of the use of Raman spectroscopy for the determination of amphibole asbestos. Mineralogical Magazine 68, 455-465

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Ross C S, Kerr P F (1932) The manganese minerals of a vein near Bald Knob, North Carolina. American Mineralogist 17, 1-18

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Roth P (2007) Grunerite. in Minerals first discovered in Switzerland and minerals named after Swiss individuals, Kristallografik Verlag (Achberg Germany) 182-183

Steel E, Wylie A (1981) Mineralogical characteristics of asbestos. 1, in Geology of Asbestos Deposits, Edwards Brothers, Inc. (Ann Arbor, MI.) 93-99

Su S C (2008) in How to use the d-spacing/interfacial angle tables to index zone-axis patterns of amphibole asbestos minerals obtained by selected area electron diffraction in transmission electron microscope, Asbestos Analysis Consulting (Newark, Delaware) 1-160

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Su S C (2003) A rapid and accurate procedure for the determination of refractive indices of regulated asbestos minerals. American Mineralogist 88, 1979-1982

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Tribaudino M, Hovis G L, Almer C, Leaman A (2022) Thermal expansion of minerals in the amphibole supergroup. American Mineralogist 107, 1302-1312

Uchida E (1983) Grunerite from the Shinyama ore deposit, Kamaishi mine, Japan. The Canadian Mineralogist 21, 517-528

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Winchell A N (1931) Further studies in the amphibole group. American Mineralogist 16, 250-266

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Yong T, Dera P, Zhang D (2019) Single-crystal X-ray diffraction of grunerite up to 25.6 GPa: a new high-pressure clinoamphibole polymorph. Physics and Chemistry of Minerals 46, 215-227

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