锑
岩相学
辉绿岩
镁橄榄石
莫来石
矿物学
矿物
熔渣(焊接)
烘烤
方石英
锑酸盐
冶金
石英
材料科学
地球化学
地质学
橄榄石
陶瓷
作者
Vincent Thiéry,Migueli Chedrewih,Gavyn Rollinson,Violeta Ramos,Jens Andersen
摘要
Towards the end of the 19th century and the early 20th century, France was the world's largest producer of antimony, especially due to the rich deposits in the Brioude-Massiac area. Even though all the mining and smelting activities are long gone, there are still some remains of those activities. The most original of those is the use of roasting slags as aggregates in former plant walls or industrial building. They are macroscopically characterised by a black or red colour with a vesicular aspect similar to natural pozzolanas. Common petrography and mineralogy tools have been used to characterise those slags: optical mineralogy, scanning electron microscopy coupled with energy dispersive spectroscopy (SEM-EDS) and X-ray diffraction (XRD). To gain an insight into their mineral complexity, a QEMSCAN map has been produced. The mineralogy is typical of high-temperature slags: cristobalite, quartz, mullite, fayalite-forsterite series and spinel. The antimony content is quite high, up to seven percent, under the form of various antimony oxides and native antimony.
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