Two types of olivine in the Dongujimqin mesosiderite were identified: the m
atrix olivine and the brecciform olivine. The electron microprobe analyses
show that there are distinct differences between two types of olivine in th
e aspects of the FeO/MnO ratio, the species of inclusion mineral, the conce
ntrations of Fe an Ni in kamacite and taenite inclusions. It indicates that
the matrix olivine was from the host meteorite and the brecciform olivine
was from the other cosmic substance. It is the collision and combination of
two cosmic substances soaring separately in cosmos that formed the Donguji
mqin mesosiderite.