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金刚石作为一种重要的矿物资源,在工业以及科技发展等方面都具有重要的作用。而金刚石成矿条件特殊,矿产稀少,继最早发现的金伯利岩型金刚石母岩后,钾镁煌斑岩因其金刚石的含矿性而广泛受到重视。本文通过分析综述钾镁煌斑岩的地球化学特征以及矿物组成特征、分类命名的依据、金刚石的成矿机制、钾镁煌斑岩与金刚石成矿的关系等方面,总结出遥感探测、物理探测、化学探测、原生矿床指示矿物等方法,为钾镁煌斑岩中金刚石的找矿提供依据。
As an important mineral resource, diamond plays an important role in industrial and technological development. The special conditions of diamond mineralization, mineral sparse, following the earliest discovery of kimberlite-type diamond-bearing rock, auriferite lamprophytes because of its diamond-bearing mineralization and widespread attention. This article summarizes the geophysical and geochemical features of the lamproas from the aspects of the geochemical characteristics, the mineral composition, the classification and nomenclature, the metallogenic mechanism of diamond, the relationship between the lamproite and the diamond mineralization. , Chemical exploration, primary mineral deposits and other methods, to provide the basis for mineral prospecting of diamond in lamproite.