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陨石是一种天然的多相矿物体系,其主要矿物如橄榄石、辉石、陨硫铁、锥纹石等都是含铁矿物。穆斯鲍尔效应方法,对于非破坏性探测铁原子在各矿物相中的分布和存在的价态等是一种很有效的手段。1964年,S.S.汉恩(Hanna)和E.L.斯普雷克尔-西格尔(sprenkel-Segal)首次对石陨石作了穆斯鲍尔谱研究,分析了其中几个主要含铁矿物相:硅酸盐相、金属相和硫化物相。以后不断有人把这一方法用于陨石研究,主要是对普通球粒陨石,也有碳质球粒陨石和无球粒陨石。还有人尝试把穆斯鲍尔效应方法用于
Meteorite is a natural multi-phase mineral system, its main minerals such as olivine, pyroxene, pyrite, cones and other iron-bearing minerals. The method of Muspeauer effect is a very effective method for non-destructive detection of the distribution and existing valence of iron atoms in various mineral phases. In 1964, for the first time, Hanna and Sprenkel-Segal performed muscourt analysis of stone meteorites and analyzed several of the major iron-bearing mineral phases: Silicate phase, metal phase and sulfide phase. Some people continue to use this method for meteorite research, mainly for ordinary chondrules, but also carbonaceous chondrules and chondrules. Others tried to use the method of Muswell-Bauer effect