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首页> 外文期刊>Mikrochimica Acta: An International Journal for Physical and Chemical Methods of Analysis >Micro-PIXE Analysis of Monazite from the Dora Maira Massif,Western Italian Alps
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Micro-PIXE Analysis of Monazite from the Dora Maira Massif,Western Italian Alps

机译:意大利西阿尔卑斯山Dora Maira地块中独居石的Micro-PIXE分析

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摘要

Quantitative micro-PIXE and electron mi-croprobe analyses,as well as micro-PIXE compositional mapping of trace elements were performed on monazite [(Ce,La,Nd,Th)PO_4] inclusions in pyrope megablasts from Dora Maira Massif,Western Italian Alps for petrological and geochronological purposes.Monazite was studied by SEM-BSE imaging and by X-ray qualitative compositional maps of major elements;further WDS electron microprobe analyses were carried out in areas showing different BSE intensity in order to quantify chemical zoning.Finally,micro-PIXE compositional maps and quantitative analyses were performed on selected spots and areas.EPMA data indicate that the Dora Maira monazite is Ce- and Th-rich with homogeneous concentrations of LREE,but with a significantly heterogeneous distribution of Th,as well as of Y,Sr,U and Pb as displayed by micro-PIXE compositional mapping.HREE mostly occur in concentrations below the detection limit for standard quantitative EPMA.Th-U-Pb zoning suggests two monazite growth events,dated at 35 (+-7 Ma) and 60 Ma (+-10 Ma),respectively.While the younger age of 35 Ma found in high-Th monazite areas corresponds to the thermal and baric peak of the UHP metamorphism in the Dora Maira Massif,in agreement with previous literature data,the older ages of 60 Ma found in low-Th areas have to be confirmed by U-Th-Pb isotopic data.
机译:在意大利西阿尔卑斯山多拉·迈拉·马西夫多拉·迈拉·马西夫的焦炉大爆炸中,独居石[(Ce,La,Nd,Th)PO_4]夹杂物上进行了微量PIXE和电子微型探针定量分析以及微量元素的微量PIXE成分映射。通过SEM-BSE成像和主要元素的X射线定性成分图对独居石进行了研究;在显示不同BSE强度的区域进行了进一步的WDS电子微探针分析,以量化化学分区。对选定的斑点和区域进行了-PIXE组成图和定量分析。EPMA数据表明,Dora Maira独居石富含铈和Th,具有均匀的LREE浓度,但Th和Y的分布明显不同微量PIXE成分图显示了Sr,U,Pb和Pb.HREE主要出现在浓度低于标准定量EPMA的检出限的情况下.Th-U-Pb分区显示两个Mo纳兹石的生长事件分别在35(+ -7 Ma)和60 Ma(+ -10 Ma)发生。虽然在高Th独居石地区发现的35 Ma的年轻年龄对应于UHP变质的热峰和重峰。在Dora Maira断层中,与以前的文献数据一致,必须通过U-Th-Pb同位素数据确认在低Th地区发现的60 Ma的年龄较大。

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