Found at sites of meteorite impact, formed by shock metamorphism of quartz at temperatures 1200 deg C and pressures »100 kbar. Quartz, tridymite, cristobalite, and coesite are polym orphs.
IMA Status:
Approved IMA 1962
Locality:
Meteor Crater, Arizona, USA. Link to MinDat.org Location Data.
Name Origin:
Named for Sergei Mikhailovich Stishov, Russian Crystallographer who, with S.V. Popova, first synthesized the compound.
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Ross N L , Shu J F , Hazen R M , Gasparik T , American Mineralogist , 75 (1990) p.739-747, High-pressure crystal chemistry of stishovite, P = 0, but in the diamond cell
CI meas= 0.102 (Poor) - where the CI = (1-KPDmeas/KC) CI calc= 0.089 (Poor) - where the CI = (1-KPDcalc/KC)
KPDcalc= 0.1894,KPDmeas= 0.1868,KC= 0.208 Ncalc = 1.89 - 1.9
Optical Data:
Uniaxial (+), w=1.799, e=1.826, bire=0.0270.
Calculated Properties of Stishovite
Electron Density:
Bulk Density (Electron Density)=4.28 gm/cc note: Specific Gravity of Stishovite =4.29 gm/cc.
Fermion Index:
Fermion Index = 0.02 Boson Index = 0.98
Photoelectric:
PEStishovite = 1.80 barns/electron U=PEStishovite x rElectron Density= 7.70 barns/cc.
Radioactivity:
GRapi = 0 (Gamma Ray American Petroleum Institute Units) Stishovite is Not Radioactive