Discovered by Rudolph L. Mössbauer in 1957, the Mössbauer effect (i.e. gamma-resonance spectroscopy) is the phenomenon of the emission or absorption of a gamma ray without loss of energy due to recoil of the nucleus and without thermal broadening. This technique has been applied to many science fields (e.g., physics, chemistry, geology, biology), since it provides information about the nuclear and electronic properties of materials. In this paper, a review of works focusing on the application of ⁵⁷Fe Mössbauer spectroscopy study of the meteoritic Fe-Ni system will be reported.

中文翻译：

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Fe-Ni陨石：^57项FeMössbauer光谱研究的回顾

罗斯伯格·默斯鲍尔（Rudolph L.Mössbauer）于1957年发现穆斯鲍尔效应（即伽马共振光谱），是一种伽马射线的发射或吸收现象，不会因原子核的反冲而造成能量损失，也不会发生热展宽。由于该技术提供了有关材料的核和电子特性的信息，因此已应用于许多科学领域（例如，物理学，化学，地质学，生物学）。在本文中，将对专注于⁵⁷ FeMössbauer光谱学在流星化Fe-Ni系统研究中的应用的工作进行综述。