首页> 外文期刊>Hyperfine Interactions: Journal Devoted to Research in the Border Regions of Solid State, Atomic and Nuclear Physics >Characterization of the Carancas–Puno meteorite by energy dispersive X-ray fluorescence, X-ray diffractometry and transmission Mossbauer spectroscopy
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Characterization of the Carancas–Puno meteorite by energy dispersive X-ray fluorescence, X-ray diffractometry and transmission Mossbauer spectroscopy

机译:能量散射X射线荧光,X射线衍射和透射莫斯鲍尔光谱表征Car肉-普诺陨石

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摘要

We report the results of the study of ameteorite that impacted an inhabited zone on 15 September 2007 in the neighborhood of the town of Carancas, Puno Region, about 1,300 km south of Lima. The analysis carried out by energy dispersive X-ray fluorescence, X-ray diffractometry and transmission Mossbauer spectroscopy (at room temperature and at 4.2 K), reveal the presence in the meteorite sample of magnetic sites assigned to taenite (Fe,Ni) and troilite (Fe,S) phases, and of two paramagnetic doublets assigned to Fe~(2+), one associated with olivine and the other to pyroxene. In accord with these results, this meteorite is classified as a type IV chondrite meteorite.
机译:我们报告了2007年9月15日对在利马以南约1300公里处普诺大区Carancas镇附近居民区的陨石研究的结果。通过能量色散X射线荧光,X射线衍射和透射莫斯鲍尔光谱仪(在室温下和4.2 K下)进行的分析表明,陨石样品中存在着分配为钛铁矿(Fe,Ni)和三叶铁矿的磁性位点(Fe,S)相,以及分配给Fe〜(2+)的两个顺磁性双峰,一个与橄榄石相关,另一个与辉石相关。根据这些结果,该陨石被归为IV型球粒陨石。

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