Thermoluminescence Study on Bo County Meteorite
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摘要: 毫县陨石于1977年10月20日下午2时30分左右降落于安徽亳县张沃公社吝子门大队.陨石表面灰黑色,有0.5mm厚的烧蚀层,具有明显的球粒结构.已查明[1]该陨石的透明矿物有镁橄榄石、贵橄榄石、透铁橄榄石、古铜辉石、顽火辉石、斜顽辉石、顽火透辉石、易变辉石、斜长石、正长石、白磷钙矿、石英、黑云母、白云母、方解石、刚玉等;不透明矿物有陨硫铁、铁纹石、镍纹石、铬铁矿、镁铁尖晶石、钛铁矿、镍黄铁矿、石墨、磁铁矿、方铁矿、自然铜和张衡矿等.经研究[1]该陨石的化学-岩石类型为LL4,属于平衡球粒陨石.Abstract: In this paper the results of thermoluminecence (TL) study on Bo County meteorite are reported. Temperature gradient in the meteorite, produced by heating during its atmospheric passage, is 34.2°C/mm in head, 24.8°C/mm in side. The temperature profiles of the meteorite is closed to the Barwell meteorite, and more reasonably consistent with the steady-state solution to the heat conductivity equation in a case of the ablation rate of 0.10 cm/sec. According to the TLcurve of the meteorite the parameter Ln (LT/HT) is 1.30. So the meteorite belong to type A.
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