Isotopic and trace element compositions of two unusual Type b inclusions from the Ningqiang carbonaceous chondrite

Lin Y., Floss C., Stadermann F. J., Zinner E. and Kimura M. (2000) Lunar and Planetary Science XXXI, Abstract #1624, Lunar and Planetary Institute, Houston (CD-ROM).


ABSTRACT

Two unusual Type B inclusions were found in the Ningqiang anomalous carbonaceous chondrite. They show large variations in melilite compositions, with åkermanite contents decreasing from 80-90 mol% in the centers of the inclusions to 4-15 mol% near the rims, suggesting that these inclusions crystallized from melts. However, both inclusions also contain fragments of fassaite, with corroded outlines and surrounded by highly Ti-Al- enriched fringes, that may be relict. Furthermore, one of the inclusions, NQJ331, may also contain relict or xenolithic grains of anorthite and palisades. The other inclusion, NQJ354, contains a grossite-bearing spinel- hibonite spherule, which crystallized from an SiO 2 - poor melt at high temperature and was injected into the Type B host. Here we report Mg isotopic and trace element measurements, undertaken in order to clarify the complex formation and evolution of both Type B inclusions.


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