Formation of the Mont Dieu IIE Non Magmatic Iron Meteorite, and Origin of its Silicate Inclusions

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Scientific paper

Mont Dieu is an IIE nonmagmatic iron meteorite showing primitive
features such as preserved chondrules and glass. SEM and geochemical
analyses demonstrate that it most likely originated from an H-chondrite
parent body impacted by a Fe-Ni projectile.

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