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Geochemical Peculiarities of Some Rock-Forming Minerals during Experimental Modeling of Shock Metamorphism

机译:冲击变质作用实验建模中某些成岩矿物的地球化学特征

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(1) REEs and minor elements, as well as major chemical components of garnets and biotites with rare exclusions are poorly sensitive to the shock influence during experimental modeling of shock metamor-phism within the abovementioned limits.rn(2) The most mobile among REEs are LREEs (La and Ce) accumulated in garnet and Gd with the concentration decreasing during shock loading. Among minor elements, Ba, Rb, Sr, and Nb crystallochemically incompatible for garnet demonstrate a tendencyrnof accumulation in this mineral. The concentrations of Ba and Cr compatible for biotite decrease as a result of the experiment.rn(3) REEs in garnet behave as three independent groups as a result of the experiment: LREEs, MREEs, and HREEs. There is no such division in biotites.
机译:(1)在上述限制范围内的冲击变质作用实验建模期间,稀土元素,石榴石和黑云母的稀土元素和微量元素以及主要化学成分对冲击影响的敏感性较弱。(2)稀土元素中最易移动的元素是石榴石和Gd中积累的LREE(La和Ce),在冲击载荷下浓度降低。在微量元素中,石榴石的晶体化学不相容的Ba,Rb,Sr和Nb在这种矿物中表现出趋势蓄积。实验结果表明,与黑云母相容的Ba和Cr浓度降低。rn(3)石榴石中的REE表现为三个独立的基团:LREE,MREE和HREE。黑云母中没有这种划分。

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  • 来源
    《Doklady Earth Sciences》 |2010年第1期|P.638-643|共6页
  • 作者单位

    Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, Saint-Petersburg;

    Geological Faculty, Moscow State University, Moscow;

    Russian Federal Nuclear Center-Zababakhin Russian Research Institute of Technological Physics, Snezhinsk;

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