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首页> 外文期刊>Central european geology >STUDY OF D34S AND CHEMICAL COMPOSITION OF SULFIDES FROM ALKALINE INTRUSION IN SE PART OF KHIBINA MASSIF (KOLA PENNISULA, N RUSSIA)
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STUDY OF D34S AND CHEMICAL COMPOSITION OF SULFIDES FROM ALKALINE INTRUSION IN SE PART OF KHIBINA MASSIF (KOLA PENNISULA, N RUSSIA)

机译:喜树碱(俄罗斯可乐半岛)SE部分碱浸入物中D34S和硫化物的化学组成的研究

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摘要

In this study we report new data on the δ~(34)S of sulfides from SE part of Khibina Massif from the northern part of Baltic Shield. The selected ore minerals were analyzed with optical and electron microscopy (Hitachi SU6600 with EDS attachment) in the Electron and Optical Microscopy Laboratory, Maria Curie-Sklodowska University (total number of analyses was 2488 and 607, respectively), whereas the δ~(34)S of sulfides from syenites of central part of the massif was determined in the Mass Spectrometry Laboratory, Maria Curie-Sklodowska University. These sulfides were analyzed by ICP MS in Department of Soil Science in order to figure out typical metallic concentrations.
机译:在这项研究中,我们报告了来自波罗的海盾北部Khibina Massif SE部分的硫化物的δ〜(34)S的新数据。选定的矿石矿物在玛丽亚·居里-斯克洛多夫斯卡大学电子和光学显微镜实验室通过光学和电子显微镜(Hitachi SU6600附有EDS)进行分析(分析总数分别为2488和607),而δ〜(34来自断层中部正长岩的硫化物的硫化物是在玛丽亚居里-斯科洛多夫斯卡大学的质谱实验室中测定的。为了确定典型的金属浓度,通过土壤科学系的ICP MS对这些硫化物进行了分析。

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