Small tabular body of nickeliferous serpentinite, probably a contact deposit, along the junction of quartzite and an ultramafic intrusive. Possibly because of a nickel-rich meteorit e impact.
IMA Status:
Approved IMA 1974
Locality:
Three km west of the Scotia talc mine, Bon Accord area, Barberton, Transvaal, South Africa. Link to MinDat.org Location Data.
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Perkins D A , Attfield J P , Journal of the Chemical Society, Chemical Communications , 1991 (1991) p.229-231, Resonant powder X-ray determination of the cation distribution in FeNi2BO5, Locality: synthetic
Physical Properties of Bonaccordite
Color:
Reddish brown.
Density:
5.17
Diaphaneity:
Opaque
Hardness:
7 - Quartz
Luster:
Vitreous - Adamantine
Streak:
brown
Optical Properties of Bonaccordite
Optical Data:
NCalc= 2.16 - from Gladstone-Dale relationship (KC = 0.2232) where Ncalc=Dcalc*KC+1 NCalc= 2.15 - from Gladstone-Dale relationship (KC = 0.2232) where Ncalc=Dmeas*KC+1
Calculated Properties of Bonaccordite
Electron Density:
Bulk Density (Electron Density)=4.99 gm/cc note: Specific Gravity of Bonaccordite =5.19 gm/cc.
Fermion Index:
Fermion Index = 0.01 Boson Index = 0.99
Photoelectric:
PEBonaccordite = 24.37 barns/electron U=PEBonaccordite x rElectron Density= 121.65 barns/cc.
Radioactivity:
GRapi = 0 (Gamma Ray American Petroleum Institute Units) Bonaccordite is Not Radioactive