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Colombian silica sands

机译:哥伦比亚硅砂

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摘要

Silice Sand Business (SSB), a Colombia-based company, has identified silica sand resources exceeding 20m. tonnes and grading 98.9 percent SiO_2 within the San Luis Valley of the Tolima State in Colombia. The silica is found within sedimentary rocks of Cretaceous to Quaternary age. The most recent deposits are alluvial in nature and consist of sandy beds intercalculated with areas of angular quartz. These deposits are irregular and are of very little thickness. Underlying these are Cretaceous grey to red shales, which are interstratified with weathered silica. Below this section are the oldest rocks in the formation, which are those of economic interest. They form part of the Guadalupe Group and are also of Cretaceous age. The deposit has an average thickness of 15 metres and is formed of a high percentage of angular quartz which is only partially weathered in the upper sections of the body. Here, the silica is characterised by brown oxidisation.
机译:哥伦比亚公司Silice Sand Business(SSB)已确定硅砂资源超过2000万。哥伦比亚托利马州圣路易斯谷地的SiO_2含量为98.9%。在白垩纪至第四纪的沉积岩中发现了二氧化硅。最近的沉积物是冲积性的,由相互交错的砂岩床和角石英区组成。这些沉积物是不规则的,并且厚度很小。这些物质的下层是白垩纪灰色至红色页岩,并与风化的二氧化硅互层。该部分下方是该地层中最古老的岩石,具有经济价值。它们属于瓜达卢佩(Guadalupe)集团,也属于白垩纪。该沉积物的平均厚度为15米,由高百分比的角质石英形成,仅在矿体的上部部分风化。在此,二氧化硅的特征在于棕色氧化。

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