The 26Al-26Mg Chronology of a Type C CAI and POIs in Ningqiang Carbonaceous Chondrite

Physics

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Scientific paper

The ^26Al-^26Mg measurements of a type C CAI and POIs in Ningqiang
carbonaceous chondrite indicate ^26Al ages of ~0 Myr and ~2.5 Myr,
repectively. They also show isotopic disturbance in plagioclse which
might occur on the parent body at >4 Myr after CAIs.

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