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Arfvedsonite Root Name Group

A group of related mineral species
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About Arfvedsonite Root Name GroupHide

Formula:
ANa2(C2+4Fe3+}Si8O22W2
The arfvedsonite minerals are sodium amphiboles defined with A(Na+K+2Ca)> 0.5 apfu and 0.5 apfu < C(Al+Fe3++2Ti) < 1.5 apfu with Fe3+ as the dominant element in the C3+ position. The individual members are defined by their dominant element in the A, C2+ and W position.
Crystal System:
Monoclinic
Name:
Named for Johan A. Arfvedson (Arfwedson) (1792-1841), Swedish chemist.
This page provides mineralogical data about Arfvedsonite Root Name Group.


Unique IdentifiersHide

Mindat ID:
8603
Long-form identifier:
mindat:1:1:8603:1

Chemistry of Arfvedsonite Root Name GroupHide

Mindat Formula:
ANa2(C2+4Fe3+}Si8O22W2

The arfvedsonite minerals are sodium amphiboles defined with A(Na+K+2Ca)> 0.5 apfu and 0.5 apfu < C(Al+Fe3++2Ti) < 1.5 apfu with Fe3+ as the dominant element in the C3+ position. The individual members are defined by their dominant element in the A, C2+ and W position.

Age distributionHide

Recorded ages:
Mesoproterozoic to Paleogene : 1456 Ma to 31.7 ± 0.7 Ma - based on 21 recorded ages.
Sample ages:
Sample IDRecorded ageGeologic TimeDating method
131.7 ± 0.7 MaOligoceneK-Ar
280.1 ± 3.1 MaLate/Upper CretaceousK-Ar
3226 ± 1.1 MaLate/Upper TriassicK-Ar
4319 ± 8 MaPennsylvanianAr-Ar
5430 ± 12 MaWenlockK-Ar
61456 to 1359 MaMesoproterozoicK-Ar

Chemical AnalysisHide

Oxide wt%:
Showing 12 of 15 analyses on this page.
 123456789101112
SiO249.33 %49.6 %53.22 %55.29 %49.48 %48.63 %51.64 %54.80 %54.25 %50.31 %51.86 %49.03 %
TiO20.40 %0.46 %0.37 %1.86 %0.47 %0.43 %0.74 %0.15 %1.08 %0.57 %0.38 %0.73 %
Al2O30.72 %1.22 %2.31 %0.21 %0.89 %0.58 %0.58 %0.17 %0.03 %0.63 %1.50 %0.87 %
Fe2O31.55 %3.77 %2.26 %11.60 %4.74 %9.84 %8.07 %12.00 %13.98 %14.51 %
FeO30.95 %33.0 %14.01 %10.52 %31.58 %24.69 %17.53 %2.61 %6.69 %22.14 %5.11 %13.70 %
MnO2.15 %0.86 %0.05 %0.25 %2.04 %1.37 %0.88 %0.11 %0.32 %0.77 %4.35 %5.46 %
MgO0.74 %0.17 %15.56 %14.02 %0.70 %0.04 %7.79 %17.44 %13.99 %8.85 %0.61 %
CaO1.01 %0.39 %2.00 %2.56 %1.02 %0.30 %1.63 %2.37 %1.16 %3.07 %0.05 %
Na2O7.07 %8.7 %8.34 %7.74 %6.93 %7.01 %6.94 %6.37 %6.33 %8.82 %7.13 %8.95 %
K2O1.81 %2.33 %0.56 %2 %1.97 %3.29 %3.41 %3.44 %5.20 %1.58 %1.10 %1.29 %
ZrO20.20 %0.02 %
Cl0.01 %0.01 %
F0.64 %0.81 %1.43 %0.36 %1.59 %2.33 %2.20 %2.31 %2.43 %2.85 %
Li2O0.05 %0.45 %0.76 %0.27 %0.6 %
H2O1.21 %1.7 %1.20 %(0.82) %
O=F-0.6 %-0.15 %-0.67 %-0.97 %-1.02 %-1.20 %
ZnO0.20 %0.06 %0.05 %0.49 %0.14 %0.90 %
Cr2O30.07 %
Total:95.93 %97.4 %97.24 %100.31 %97.34 %100.5 %98.06 %99.7 %99.37 %99.41 %99.15 %98.35 %
Empirical formulas:
Sample IDEmpirical Formula
2(Na0.62K0.47) 1.09 (Na1.93Ca0.07) 2.00 (Fe2+3.43Mg0.04Fe3+0.97Mn0.12Ti0.06Al0.15Zr0.01) 4.78(Si7.92 Al0.08) 8.00 O22[ (OH) 1.97 F0.03] 2.00
13(Na0,71K0,301) 1,011 (Na1,618Ca0,382) 2 (Fe2+3,869Fe3+0,664Ti0,27Mn0,115Al0,072) 4,99 (Si7,891Al0,109) 8O22 ((OH) 1,458O0,542) 2
4(Na0.569K0.369)0.938 (Na1.603Ca0.397)2(Mg3.025Feii1.273FeIII0.411Ti0.202Al0.036Mnii0.031Li0.029)5.007Si8.002O22 ((OH)1,168F0,655O0.168)2
6(K0.67Na0.22) 0.89(Na1.95Ca0.05) 2.00 (Fe2+ 3.29Fe3+ 1.26Li0.29Mn0.19Ti0.05Zn0.02Mg0.01) 5.11(Si7.76Fe3+ 0.13Al0.11) 8.00 O22[(OH) 1.81F0.18] 1.99
14(K0.73Na0.27) 1.00 (Na2.00Ca0.01) 2.01 (Fe2+ 1.77 Mg1.10Fe3+ 0.98Li0.45Mn0.42Ti0.09Zn0.01 Al0.09) 4.91Si8.09O22[(OH) 1.41F0.59] 2.00
7(K0.67Na0.33) 1.00 (Na1.74Ca0.27) 2.01 (Fe2+ 2.26 Mg1.79Fe3+ 0.55Mn0.25Ti0.09Zn0.01 Al0.05) 5.00(Si7.94 Al0.06) 8.00O22[(OH) 1.23F0.77] 2.00
8(K0.63 Na0.15) 0.78 (Na1.62Ca0.36Mn0.02) 2.00 (Mg3.72 Fe2+ 0.31 Fe3+ 0.95Mn0.00Ti0.02Al0.00) 5.00(Si7.85Al0.03 Fe3+ 0.11Cr0.01) 8.00O22[F1.06(OH) 0.94]2.00
9K0.98 (Na1.81Ca0.18) 1.99 (Mg3.07 Fe2+ 0.83 Fe3+ 0.90Mn0.04Ti0.12Zn0.01 Al0.01) 4.98Si8.00)O22[F1.03(OH) 0.73O 0.24] 2.00
10(K0.32Na0.68)Na2(Li0.48Fe2.83Mn0.1Zn0.06Fe1.46Ti0.07)(Si7.88Al0.12)O22(F1.15OH0.85)
15(K0.25Na0.75)Na2(Li0.48Fe2.84Mn0.11Zn0.05Fe1.45Ti0.07)(Si7.89Al0.11)O22(F1.35OH0.65)
11A(Na0.526K0.207)B0.733( (Na1.514Ca0.485Mn0.072) C2.00( (Mg2.057Li0.160Fe2+0.631Mn2+0.544Zn0.015Fe3+1.552Ti0.042) 5.001 T( (Si7.652Al0.261) 7.913OW22( (F1.143(OH) 0.857) 2.00
12A(Na0.767K0.261)B1.028( (Na1.990Ca0.010)C2.00( (Mg0.144Li0.383Fe2+1.818Mn2+0.734Fe3+1.733Ti0.087) 5.004 T( (Si7.780Al0.163) 7.943OW22( (F1.448(OH) 0.552) 2.00
Sample references:
IDTypeLocalityReferenceNotes
1Motzfeldt Centre, Igaliku Complex, Kujalleq, GreenlandSample from an alkali-rich syenite.
2ILM42Ilímaussaq complex, Kujalleq, GreenlandThe sample was collected from ilvaite bearing endoskarns formed by late-magmatic to hydrothermal veins on the south coast of the Tunulliarfik fjord. Mineral compositions were analyzed using a JEOL 8900 electron microprobe
3Mud Tank Vermiculite Mine, Alcoota Station, Central Desert Region, Northern Territory, AustraliaAverage of 6 analyses. Sample taken from a silicate rich carbonatite.
4760Coyote Peak, Humboldt County, California, USAAnalyzed by single crystal X-ray and electron- and ion-microprobe techniques. The sample is also analyzed for Li and H.
5Motzfeldt Centre, Igaliku Complex, Kujalleq, GreenlandSample from an alkali-rich syenite.
6Type SpecimenPotassic-Arfvedsonite occurrence, Pegmatite Valley, Lilleelv, Head of Kangerluarsuk, Kangerluarsuk Fjord, Ilímaussaq complex, Kujalleq, GreenlandThe chemical composition of potassicarfvedsonite was obtained (fluorine and cations except Li) by a Camebax SX50 electron microprobe. Li was determined by atom emission using a Carl Zeiss AAS30 spectrophotometer. The water content was determined by the Alimarin method, a modified Penfield, with water absorption by Mg(ClO4)2. The Fe2+/ Fe3+ ratio was determined via Mössbauer spectroscopy. Single-crystal diffraction data were collected at room temperature using a Nonius Kappa CCD diffractometer. X-ray powder diffraction data were obtained using a DRON UM-1 diffractometer and Fe-filtered CoKα-radiation
7Hilairitovoye pegmatite, 252 m level, Kirovskii apatite mine, Kukisvumchorr Mt, Murmansk Oblast, RussiaThe chemical composition of potassicarfvedsonite was obtained (fluorine and cations except Li) by a Camebax SX50 electron microprobe. Li was determined by atom emission using a Carl Zeiss AAS30 spectrophotometer. The water content calculated The Fe2+/ Fe3+ ratio was calculated.
8Type SpecimenHighway 366 roadcut, Val-des-Monts, Les Collines-de-l'Outaouais RCM, Outaouais, Québec, CanadaThe sample were analyzed at Virginia Polytechnic Institute by wavelength dispersion, using a 9-channel ARL - SEMQ microprobe.Fe2+/Fe3+ ratio were found by by Mossbauer spectroscopy. The cell parameters were determined from single-crystal X-ray powder-diffraction data.
9AS04-36Monte Metocha, Xixano, Montepuez District, Cabo Delgado Province, MozambiqueThe sample was analyzed by electron microprobe using a Cameca SX-100 operating in wavelength-dispersive mode. The powder-diffraction pattern was recorded from a small fragment on a 114.6 mm Debye-Scherrer powder camera with a Gandolfi attachment and Ni-filtered Cu-Ka X-radiation The Fe2+-Fe3+ ratio and the H2O content were derived from the results of crystal-structure refinement. The oxo component (O2 at the O(3) site) was estimated based on the Ti content.
10H1Hurricane Mountain localities, North Conway, Conway, Carroll County, New Hampshire, USAChemical and structural analysis including site assignments. See reference for details.
11830C30-5Virgin Canyon pluton, Questa, Taos County, New Mexico, USAA single crystal about 0.2x2mm was analyzed with EMPA, XRD and site scattering techniques. Li is ordered at M3, which is compensated by Fe3+ in the M2 site. The sample is named magesio-ferri-fluoro-katophorite in the references, but as #B#Na>1.5 and M#3+# > 1,5, the composition corresponds to fluoro-arfvedsonite.
12Q83J70-3  "  "A single crystal about 0.2x2mm was analyzed with EMPA, XRD and site scattering techniques. Li is ordered at M3, which is compensated by Fe3+ in the M2 site.
13Mount Rittmann, Victoria Land, East Antarctica, AntarcticaRepresentative sample of amphibole from the groundmass of hyperalkaline volcanic rocks. The analysis was performed with an EDAX system mmounted on a Electronic Micropscope Phillips SEM-500. Analysis is normalized using Locock (2014)
14Palitra pegmatite, Karnasurt mine, Karnasurt Mountain, Lovozersky District, Murmansk Oblast, RussiaThe chemical composition of potassicarfvedsonite was obtained (fluorine and cations except Li) by a Camebax SX50 electron microprobe. Li was determined by atom emission using a Carl Zeiss AAS30 spectrophotometer. The water content calculated The Fe2+/ Fe3+ ratio was calculated.
15H2Hurricane Mountain localities, North Conway, Conway, Carroll County, New Hampshire, USAChemical and structural analysis including site assignments. See reference for details.

Crystallography of Arfvedsonite Root Name GroupHide

Crystal System:
Monoclinic

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0020742Magnesio-arfvedsoniteOberti R, Boiocchi M, Hawthorne F C, Ball N A, Harlow G E (2015) Magnesio-arfvedsonite from Jade mine tract, Myanmar: mineral description and crystal chemistry Mineralogical Magazine 79 253-2602015Jade mine tract, Myanmar0293
0001597ArfvedsoniteHawthorne F C, Ungaretti L, Oberti R, Bottazzi P, Czamanske G K (1993) Li: an important component in igneous alkali amphiboles American Mineralogist 78 733-7451993Questa caldera, New Mexico0293
0001598ArfvedsoniteHawthorne F C, Ungaretti L, Oberti R, Bottazzi P, Czamanske G K (1993) Li: an important component in igneous alkali amphiboles American Mineralogist 78 733-74519930293
0007427Magnesio-arfvedsoniteGhose S, Kersten M, Langer K, Rossi G, Ungaretti L (1986) Crystal field spectra and Jahn Teller effect of Mn3+ in clinopyroxene and clinoamphiboles from India Physics and Chemistry of Minerals 13 291-30519860293
0005126ArfvedsoniteHawthorne F C (1976) The crystal chemistry of the amphiboles: V. The structure and chemistry of arfvedsonite The Canadian Mineralogist 14 346-35619760293
CIF Raw Data - click here to close

Relationship of Arfvedsonite Root Name Group to other SpeciesHide

Other Members of Sodium Amphibole Subgroup:
Eckermannite Root Name GroupANa2(C2+4Al}Si8O22W2Mon.
Glaucophane Root Name Group◻Na2(C2+3Al2)Si8O22W2Mon.
Leakeite Root Name GroupANa2(C2+2C3+2Li)(Si8O22)W2
Nybøite Root Name GroupANa2(C2+3C3+2)(AlSi7O22)W2
Riebeckite Root Name Group◻Na2(C2+3Fe3+2)(Si8O22)W2Mon.
Arfvedsonite Root Name Group Members:
Arfvedsonite NaNa2(Fe2+4Fe3+)Si8O22(OH)2Mon. 2/m : B2/m
'Fluoro-arfvedsonite' NaNa2(Fe2+4Fe3+)Si8O22F2
Magnesio-arfvedsonite NaNa2(Mg4Fe3+)(Si8O22)(OH)2Mon. 2/m : B2/m
Magnesio-fluoro-arfvedsonite NaNa2(Mg4Fe3+)[Si8O22]F2Mon. 2/m : B2/m
Potassic-arfvedsonite KNa2(Fe2+4Fe3+)(Si8O22)(OH)2Mon. 2/m : B2/m
Potassic-magnesio-arfvedsonite KNa2(Mg4Fe3+)(Si8O22)(OH)2Mon. 2/m : B2/m
Potassic-magnesio-fluoro-arfvedsonite KNa2(Mg4Fe3+)(Si8O22)F2Mon. 2/m : B2/m
Click on any node to view relationships. Formula-derived relationship network for the group members above. Use Find related species to add formula-neighbour species outside the current group view. Solid links show inferred chemical differences; dashed violet links show same-formula crystallographic differences. Hydration states are not treated as relationship changes. These relationships do not imply any real-world substitution reactions between these species.

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Arfvedsonite Root Name Group in petrologyHide

Internet Links for Arfvedsonite Root Name GroupHide

References for Arfvedsonite Root Name GroupHide

 
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