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Mellini, Marcello, Zussman, Jack (1986) Carlosturanite (not ‘picrolite’) from Taberg, Sweden. Mineralogical Magazine, 50 (358) 675-679 doi:10.1180/minmag.1986.050.358.14

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Reference TypeJournal (article/letter/editorial)
TitleCarlosturanite (not ‘picrolite’) from Taberg, Sweden
JournalMineralogical MagazineISSN0026-461X
AuthorsMellini, MarcelloAuthor
Zussman, JackAuthor
Year1986 (December)Volume50
Issue358
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_50/50-358-675.pdf+
DOIdoi:10.1180/minmag.1986.050.358.14Search in ResearchGate
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Mindat Ref. ID3913Long-form Identifiermindat:1:5:3913:4
GUID0
Full ReferenceMellini, Marcello, Zussman, Jack (1986) Carlosturanite (not ‘picrolite’) from Taberg, Sweden. Mineralogical Magazine, 50 (358) 675-679 doi:10.1180/minmag.1986.050.358.14
Plain TextMellini, Marcello, Zussman, Jack (1986) Carlosturanite (not ‘picrolite’) from Taberg, Sweden. Mineralogical Magazine, 50 (358) 675-679 doi:10.1180/minmag.1986.050.358.14
In(1986, December) Mineralogical Magazine Vol. 50 (358) Mineralogical Society
Abstract/NotesAbstractThe second occurrence of the asbestiform silicate carlosturanite is reported. The mineral occurs in Taberg, Sweden, and it was previously reported as ‘picrolite’, that is fibrous antigorite. Carlosturanite from Taberg is non-pleochroic, green in colour and has positive optical elongation. The unit cell parameters are a = 36.55, b = 9.31, c = 7.27Å, β = 101.05°. Based on the determined formula, (Mg20.47Fe0.59Mn0.06Cr0.01Ti0.01) (Si11.68Al0.28)O27.81(OH)34.19H2O carlosturanite can be expected to crystallize within the pure MgO-SiO2-H2O system as a low-grade metamorphic mineral.Because there are close similarities in structure and properties of carlosturanite and the picrolite variety of antigorite, their distinction requires careful attention to X-ray and electron diffraction patterns and chemical compositions. The present identification of the Taberg specimen as carlosturanite puts a lower limit of 33.7 Å to the known range of a parameters of antigorite.


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