山东省平邑县大井头钾镁煌斑岩地质特征及金刚石含矿性

    A discussion on geological characteristics and diamond ore-bearing potentiality of the Dajingtou lamporphite, Pingyi County, Shandong Province

    • 摘要: 平邑县大井头岩体发现以来,其岩性界定和金刚石含矿性始终悬而未解。近期针对其深部施工2个钻孔,在钻孔人工重砂样中选获原生金刚石3颗。结合岩矿鉴定、岩石地球化学和重砂矿物特征,认为大井头岩体为含金刚石的钾镁煌斑岩管,岩体下游的金刚石及其重砂矿物异常应由该岩体引起。结合周边存在的金刚石指示矿物异常和多处尚未查明的疑似岩体,认为该地区具有广阔的金刚石原生矿找矿前景。

       

      Abstract: Since the discovery of the Dajingtou volcanic rock in Pingyi County, the problem of its lithology and the ore-bearing potentiality of diamond has not been solved. Recently, two boreholes unveiled fresh spotted rocks at the depth of 580m or so, and three diamonds were selected from them. According to the rock features, lithogeochemistry and heavy mineral characteristics, it is considered that the Dajingtou volcanic rock is lamproite-bearing diamond, which might have caused the anomalies of diamonds and heavy minerals in the lower reaches of the tube. Combined with a number of suspected lamprophyre exposed in surrounding areas, it is considered that there is a great potential for primary diamond ore.

       

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