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Mineral phases on the fracture of a glass particle and in the fines of a Luna 24 regolith sample

机译:玻璃颗粒断裂和Luna 24重磨石样品细粒中的矿物相

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摘要

This paper reports new findings of native molybdenum and iron from Mare Crisium. Native tin, copper, and nickel were detected for the first time in this area of the lunar surface. Native tantalum and indium, intermetallic compound Ta2Mo, and barium titanate Ba2TiO4 were found for the first time on the Moon. The latter two phases were observed for the first time in nature. It was shown that the investigated mineral phases correspond to different genetic groups (preimpact, impact, and postimpact mineral assemblages), which is in general typical of lunar regolith. Based on the morphological features of the identified mineral phases, the history of the formation of impact glass particles was reconstructed in part. They were probably affected by at least three impact events. It was concluded that the peculiar molybdenum geochemical anomaly observed in a group of orange impact glass fragments was not related to the impactor material but rather to the intrinsic enrichment in molybdenum of lunar rocks (target) in the area of the impact events. It was supposed that this enrichment could be of exhalative (fumarole) nature.
机译:本文报道了来自母马Cri的天然钼和铁的新发现。在月球表面的该区域首次检测到天然锡,铜和镍。首次在月球上发现了天然钽和铟,金属间化合物Ta2Mo和钛酸钡Ba2TiO4。自然界中第一次观察到后两个阶段。结果表明,所研究的矿物相对应于不同的遗传族群(撞击前,撞击和撞击后的矿物组合),这通常是月球变石的典型特征。根据确定的矿物相的形态特征,部分重建了冲击玻璃颗粒的形成历史。他们可能受到至少三个影响事件的影响。结论是,在一组橙色撞击玻璃碎片中观察到的独特的钼地球化学异常与撞击器材料无关,而是与撞击事件区域内月球岩石(目标)中钼的固有富集有关。据认为,这种浓缩可能具有呼气性(富马烯)性质。

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