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新疆浅水河烧变岩矿床的地质特征及开发应用 被引量:3

Geological Characteristics of the Qianshuihe Deposit of Burnt Stone in Xinjiang and Its Exploitation and Utilization
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摘要 烧变岩是煤层自燃产生的高温,对周围岩层的烧烤作用所形成的一种变质岩。赋存在侏罗系含煤地层的上部。工业类型为人工火山灰质烧粘土混合材。焙烧高岭土、火烧角砾岩、火烧岩、烧变泥岩四种矿石自然类型。烧变岩的特殊物化性能,广泛地应用于水泥混合材、铝质校正原料、耐火材料、园林观赏石。 Burnt stone is a metamorphic rock that is formed by baking of the country rocks with the high-temperature heat naturally produced from coal beds.The deposit occurs in the upper part of the Jurassic coal-bearing strata.In terms of industrial type,burnt stone is a burnt clay mixed material of artificial volcanic ash.Its natural types are roasted kaolin, burnt breccia,burnt rock and burnt mudstone.Due to its special physical and chemical pro- perties,the burnt stone can be widely applied to mixed material for cement,aluminous material and refractory material and as ornamental stone in gardening.
作者 王尤宏
出处 《建材地质》 1993年第1期21-25,共5页
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