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首页> 外文期刊>Doklady Earth Sciences >The Na-Mg-Fe-Ti Oxide Mineral in Association with Picroilmenite and Freudenbergite from Kimberlite of the AK8 Pipe, Botswana (Natural and Experimental Data)
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The Na-Mg-Fe-Ti Oxide Mineral in Association with Picroilmenite and Freudenbergite from Kimberlite of the AK8 Pipe, Botswana (Natural and Experimental Data)

机译:博茨瓦纳AK8管道金伯利岩中的Na-Mg-Fe-Ti氧化物矿物与青铜铁矿和Freudenbergite结合(自然和实验数据)

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摘要

The previously unknown Na-Mg-Fe-Ti oxide mineral of the idealized composition Na-4MgFe_2~(3+)Ti_5O_16 was discovered in altered areas of picroilmenite ((Fe, Mg)TiO_3) xenocrysts in association with freudenbergite (Na_2(Ti, Fe)_8O_(16))) in porphyric kimberlite of the AK8 pipe in the Orapa kimberlite field (Botswana). According to the classification of a South African geologists, the AK8 pipe is composed of kimberlite of group I. This rock consists of serpentinized olivine phenocrysts, rarely phlogopite and picroilmenite, as well as chrome-diopside and garnet cemented by fine-granular carbonate-serpentine aggregate with micro-grains of ore minerals. Secondary mineralization of the metasomatic type represented by freudenbergite and Na-Mg-Fe-Ti oxide is observed in fractures and rims on picroilmenite xenocrysts from the AK8 pipe.
机译:理想的组成为Na-4MgFe_2〜(3+)Ti_5O_16的Na-Mg-Fe-Ti氧化物矿物,在与钛铁锰矿(Na_2(Ti, Fe)_8O_(16)))在Orapa金伯利岩田(博茨瓦纳)的AK8管道的斑状金伯利岩中。根据南非地质学家的分类,AK8管道由第一类金伯利岩组成。该岩石由蛇纹石化的橄榄石隐晶石,极少的金云母和青铜石组成,以及由细粒碳酸盐-蛇纹石胶结的铬透辉石和石榴石。与矿物质的微颗粒聚集。在AK8管道中的软锰铁矿异晶体的裂缝和边缘中,观察到了以Freudenbergite和Na-Mg-Fe-Ti氧化物为代表的交代型次生矿化。

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  • 来源
    《Doklady Earth Sciences》 |2013年第2期|849-854|共6页
  • 作者单位

    Geological Faculty, Moscow State University, Moscow, Russia;

    Geological Faculty, Moscow State University, Moscow, Russia;

    Institute of Experimental Mineralogy, Russian Academy of Sciences, Moscow oblast, Chernogolovka, Russia;

    Geological Faculty, Moscow State University, Moscow, Russia;

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