首页> 外文期刊>Transactions of the Institutions of Mining and Metallurgy, Section B. Applied Earth Science >A major swarm of 'lamprophyric' dykes exposed in platinum mines of the Bushveld Complex, South Africa: geochronology, petrology and mineral chemistry
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A major swarm of 'lamprophyric' dykes exposed in platinum mines of the Bushveld Complex, South Africa: geochronology, petrology and mineral chemistry

机译:在南非的Bushveld Complex的铂金矿中暴露在铂金矿的一个主要群体:地理学,岩石学和矿物化学

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摘要

Here we document a major swarm of 'lamprophyric' dykes cross-cutting portions of the 2.06 Ga Bushveld Complex. The dykes are mostly blind at surface but exposed by underground platinum mining operations in the Rustenburg Layered Suite of the Bushveld Complex, providing a unique subsurface insight into the magnitude of the swarm. The dykes predominantly strike WNW-ESE and fall along subparallel anastomosing sets in plan view. Most dykes range from 0.5 to 2 m in true width, sometimes with millimetre-scale veinlets as off-shooting networks. The dykes bifurcate and anastomose at various scales in plan view. All dykes are vertical/subvertical and the margins may be chilled, often foliated, with lineations defined by alignment of mica crystals. Abrupt changes in mineral abundance are often recognisable as bands across a single dyke, demonstrating their compound nature. Dykes can appear 'stepped' in cross-section, sometimes with accumulations of olivine macrocrysts and/or crus-tal xenoliths located within these steps (typically of Transvaal Supergroup sediments and Bushveld lithologies).
机译:在这里,我们记录了2.06 Ga Bushveld杂岩横切部分的一大群“煌斑岩”岩墙。这些堤坝大部分是地表盲堤,但暴露在布什维尔德杂岩勒斯滕堡层状岩套的地下铂矿开采作业中,提供了对岩群规模的独特地下洞察。在平面图中,堤坝主要走向WNW-ESE,并沿着近平行的网状组落下。大多数堤坝的实际宽度在0.5到2米之间,有时带有毫米级细脉作为离射网络。在平面图中,堤坝以不同的比例分叉和吻合。所有岩墙都是垂直的/近垂直的,边缘可能会变冷,通常为叶状,线理由云母晶体排列确定。矿物丰度的突然变化通常可以识别为跨越单一堤坝的条带,这表明了它们的复合性质。岩墙在横截面上可能呈“阶梯状”,有时在这些阶梯内会聚集橄榄石大晶体和/或碎屑捕虏体(通常为Transvaal超群沉积物和Bushveld岩性)。

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