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单词 manganaxinite
释义

manganaxiniten.

Brit. /maŋɡəˈnaksᵻnʌɪt/, U.S. /ˌmæŋɡəˈnæksəˌnaɪt/
Origin: A borrowing from German. Etymon: German Manganaxinit.
Etymology: < German Manganaxinit (J. Fromme 1909, in Tschermaks mineralogische und petrographische Mitteilungen 28 311) < Mangan (see mangan- comb. form) + Axinit axinite n.
Mineralogy.
A mineral of the axinite group, Ca2Mn2+Al2BSi4O15OH, which crystallizes in the triclinic system, and occurs in pegmatite formations. More generally: an axinite with a composition near to this, spec. one with a high proportion of calcium, and with a greater proportion of manganese than iron.
ΘΚΠ
the world > the earth > minerals > types of mineral > silicates > cyclosilicates > [noun] > axinite
thumerstone1794
axinite1802
yanolite1850
thumite1868
manganaxinite1910
tinzenite1924
1910 Mineral. Mag. 15 425 Manganaxinite..Axinite rich in manganese (MnO, 11·54 per cent.) from the Harz.
1968 Amer. Mineralogist 53 1407 A suggested nomenclature of axinites, based on a triangular diagram of pure Ca-, Mn-, (Fe,Mg)- molecules, has been approved by the New Minerals and Mineral Names Commission of the IMA. It proposes that..(2)‘ferroaxinite’ be used for the end-member HCa2FeAl2BSi4O16 and for those axinites in which Ca>1.5 and Fe>Mn; (3) ‘manganaxinite’ be used for the end-member HCa2MnAl2BSi4O16 and for those axinites with Ca>1.5 and Mn>Fe; (4) the name 'tinzenite' be used for those axinites with Ca<1.5 and Mn>Fe.
1972 Amer. Mineralogist 57 989 (heading) Manganaxinite from the Mesabi Range, Minnesota.
1992 W. A. Deer et al. Introd. Rock-forming Minerals (ed. 2) 139 There is a rise in refractive indices from magnesioaxinite to ferroaxinite and through to manganaxinite, with those of tinzenite being higher still; density varies in a similar fashion.
1996 Jrnl. Metamorphic Geol. 14 125 (title) Porphyroblastic manganaxinite metapelagites with incipient garnet in prehnite-pumpellyite facies, near Meyers Pass, Torlesse Terrane, New Zealand.
This is a new entry (OED Third Edition, September 2000; most recently modified version published online March 2022).
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n.1910
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