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Wikipedia

Clinozoisite

Clinozoisite is a complex calcium aluminium sorosilicate mineral with formula: Ca2Al3(Si2O7)(SiO4)O(OH). It forms a continuous solid solution series with epidote by substitution of iron(III) in the aluminium (m3 site) and is also called aluminium epidote.[2]

Clinozoisite
Clinozoisite
General
CategorySorosilicates
Epidote group
Formula
(repeating unit)
Ca2Al3(Si2O7)(SiO4)O(OH)
IMA symbolCzo[1]
Strunz classification9.BG.05a
Dana classification58.2.1a.4
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupP21/m
Unit cella = 8.879, b = 5.583
c = 10.155 [Å]; β = 115.50°; Z = 2
Identification
ColorColorless, green, gray, light green, yellow green, pink
Crystal habitElongated primatic crystals, striated; granular to fibrous
TwinningLamellar on {100} uncommon
CleavagePerfect on {001}
FractureIrregular/uneven
TenacityBrittle
Mohs scale hardness6–7
LusterVitreous
StreakGrayish white
DiaphaneityTransparent to translucent
Specific gravity3.3–3.4
Optical propertiesBiaxial (+)
Refractive indexnα = 1.706 – 1.724 nβ = 1.708 – 1.729 nγ = 1.712 – 1.735
Birefringenceδ = 0.006 – 0.011
2V angle14 to 90° measured
References[2][3][4]

Clinothulite is a manganese bearing variety with a pinkish hue due to substitution of Mn(III) in the aluminium site.[5]

It was originally discovered in 1896 in East Tyrol, Austria, and is so-named because of its resemblance to zoisite and its monoclinic crystal structure.[2]

It occurs in rocks which have undergone low to medium grade regional metamorphism and in contact metamorphism of high calcium sedimentary rocks. It also occurs in saussurite alteration of plagioclase.[3]

Jadeite bearing pyroxene minerals have suggested clinozoisite and paragonite are associated and derived from lawsonite releasing quartz and water via the following reaction:[6]

References edit

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ a b c Clinozoisite on Mindat.org
  3. ^ a b (PDF). Archived from the original (PDF) on 2015-09-24. Retrieved 2014-03-24.
  4. ^ Clinozoisite data on Webmineral
  5. ^ Clinothulite on Mindat
  6. ^ Deer, William A. (1997). Single-chain Silicates, Volume 2A. Geological Society of London. p. 477.
  • Nesse, William D., "Introduction to Mineralogy," (c)2000 Oxford University Press ISBN 0-19-510691-1


clinozoisite, complex, calcium, aluminium, sorosilicate, mineral, with, formula, ca2al3, si2o7, sio4, forms, continuous, solid, solution, series, with, epidote, substitution, iron, aluminium, site, also, called, aluminium, epidote, generalcategorysorosilicates. Clinozoisite is a complex calcium aluminium sorosilicate mineral with formula Ca2Al3 Si2O7 SiO4 O OH It forms a continuous solid solution series with epidote by substitution of iron III in the aluminium m3 site and is also called aluminium epidote 2 ClinozoisiteClinozoisiteGeneralCategorySorosilicates Epidote groupFormula repeating unit Ca2Al3 Si2O7 SiO4 O OH IMA symbolCzo 1 Strunz classification9 BG 05aDana classification58 2 1a 4Crystal systemMonoclinicCrystal classPrismatic 2 m same H M symbol Space groupP21 mUnit cella 8 879 b 5 583 c 10 155 A b 115 50 Z 2IdentificationColorColorless green gray light green yellow green pinkCrystal habitElongated primatic crystals striated granular to fibrousTwinningLamellar on 100 uncommonCleavagePerfect on 001 FractureIrregular unevenTenacityBrittleMohs scale hardness6 7LusterVitreousStreakGrayish whiteDiaphaneityTransparent to translucentSpecific gravity3 3 3 4Optical propertiesBiaxial Refractive indexna 1 706 1 724 nb 1 708 1 729 ng 1 712 1 735Birefringenced 0 006 0 0112V angle14 to 90 measuredReferences 2 3 4 Clinothulite is a manganese bearing variety with a pinkish hue due to substitution of Mn III in the aluminium site 5 It was originally discovered in 1896 in East Tyrol Austria and is so named because of its resemblance to zoisite and its monoclinic crystal structure 2 It occurs in rocks which have undergone low to medium grade regional metamorphism and in contact metamorphism of high calcium sedimentary rocks It also occurs in saussurite alteration of plagioclase 3 Jadeite bearing pyroxene minerals have suggested clinozoisite and paragonite are associated and derived from lawsonite releasing quartz and water via the following reaction 6 4 CaAl 2 Si 2 O 8 H 2 O 2 NaAlSi 2 O 6 2 Ca 2 Al 3 Si 3 O 12 OH NaAl 3 Si 3 O 10 OH 2 SiO 2 6 H 2 O displaystyle ce 4CaAl2Si2O8 H2O 2 NaAlSi2O6 lt gt 2Ca2Al3Si3O12 OH NaAl3Si3O10 OH 2 SiO2 6H2O References edit Warr L N 2021 IMA CNMNC approved mineral symbols Mineralogical Magazine 85 3 291 320 Bibcode 2021MinM 85 291W doi 10 1180 mgm 2021 43 S2CID 235729616 a b c Clinozoisite on Mindat org a b Clinozoisite in the Handbook of Mineralogy PDF Archived from the original PDF on 2015 09 24 Retrieved 2014 03 24 Clinozoisite data on Webmineral Clinothulite on Mindat Deer William A 1997 Single chain Silicates Volume 2A Geological Society of London p 477 Nesse William D Introduction to Mineralogy c 2000 Oxford University Press ISBN 0 19 510691 1 nbsp This article about a specific silicate mineral is a stub You can help Wikipedia by expanding it vte Retrieved from https en wikipedia org w index php title Clinozoisite amp oldid 1194552964, wikipedia, wiki, book, books, library,

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