摘要
The Boxian meteorite (LL3-4), fallen in October 1977, possesses low degree of thermal metamorphism and good chondrule texture. A Ca-Al-rich chondrule （CA chondrule） was found in this chondrite. This chondrule is ca. 0.36 mm in diame ter. There is only one light red euhedral spinel crystal, ca. 34％ in volume of this chondrule, while prismatic fassaite crystals occupy ca. 29％ and only one small crystal of olivine and light brown intergranular glass of the above minerals, ca. 37％ （Fig. 1）.
