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Contents

   



(Top)
 


1 Composition and classification  





2 References  





3 See also  














Lac Dodon






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Coordinates: 45°5700N 73°5500W / 45.95000°N 73.91667°W / 45.95000; -73.91667
 

From Wikipedia, the free encyclopedia
 


Lac Dodon
TypeIron
Structural classificationCoarse octahedrite
GroupIAB complex[1]
Composition91% Fe, 8.64% Ni, 71 ppm Ga, 377 ppm Ge, 3.30 ppm Ir
CountryCanada
RegionQuebec, Canada
Coordinates45°57′00N 73°55′00W / 45.95000°N 73.91667°W / 45.95000; -73.91667
Observed fallno
Found date1993
TKW0.8 kilograms (1.8 lb)[1]

Lac Dodon is an iron meteorite discovered by Roland Octerneau of Montreal on rural private property near Lac Dodon, Saint-Calixte, Quebec.[1][2]

The recovered fragment measures approximately 10 centimetres (3.9 in) x 5 centimetres (2.0 in) x 6 centimetres (2.4 in). The meteorite was oxidized on its exterior and lying at the surface of the ground.

Composition and classification[edit]

The meteorite is a coarse octahedrite (mean bandwidth 1.34mm) with narrow cloudy taenite bands separating the kamacite lamellae. Occasional areas of coarse to fine acicular plessite and net plessite are Neumann lines and rhabdites. Sparsely developed Brezina lamellae and fine-grained globular schreibersite are present. At one exterior surface, a heat-affected zone 0.1mm thick containing unequilibrated alpha(sub)2-kamacite is preserved. Cloudy taenite extending into this zone has developed bainitic texture. The presence of the zone suggests a relatively recent fall.

References[edit]

  • ^ Kissin,S. A.; Herd, R. K., 1995, Two New Iron Meteorites from the Province of Quebec, Canada, Meteoritics, vol. 30,no. 5, page 527
  • See also[edit]


  • t
  • e

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Lac_Dodon&oldid=1091852723"

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    This page was last edited on 6 June 2022, at 19:48 (UTC).

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