Météorite pallasite
- Météorite pallasite
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Nommées en l'honneur du naturaliste allemand Pallas.
Elles sont composées de cristaux d'olivine automorphe ou xénomorphe, inclus dans une matrice de ferro-nickel où l'on retrouve souvent les figures de Widmanstätten (densité : de 4,5 à 7).
Sciées et polies, elles deviennent très esthétiques et prennent une grande valeur marchande du fait de leur rareté (1 % des chutes de météorites).
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Coupe de Pallasite - Chute d'Esquel (Argentine) exposé au Royal Ontario Museum.
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Coupe de la météorite d'Esquel
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Coupe de la météorite de Bahin (Biélorussie)
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Météorite de Brenham (USA-Texas)
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