高精度磁测寻找隐伏伟晶岩型锂矿体适用性研究——以甲基卡超大型锂矿为例

    • 摘要: 近年来磁法勘探在寻找隐伏伟晶岩脉与深部找矿预测等方面取得了较好的效果,而地面高精度磁测在伟晶岩型锂辉石矿勘探中的作用常常被忽视。为了研究地面高精度磁测在寻找隐伏矿体中的适用性,本文以甲基卡矿区为例,选取矿区代表性岩石标本进行磁性参数测量。研究表明,甲基卡矿区内岩石和矿石的磁性整体较弱,但局部地区存在高磁化率和剩余磁化强度。1: 5万地磁异常特征显示甲基卡穹窿区存在一系列中强正异常或负异常,且与伟晶岩脉相关。1: 5000磁测剖面数据进一步证实这些异常主要由地下深部地质因素引起。综合分析认为,甲基卡矿区的地磁场特征与穹窿区外明显不同,地面高精度磁测在伟晶岩型锂辉石矿勘探中具有重要作用,不能因锂辉石矿无磁性而忽视其应用潜力,同时也对类似矿床的找矿工作具有一定的借鉴意义。

       

      Abstract: In recent years, magnetic exploration has achieved good results in finding hidden pegmatite veins and deep prospecting prediction, but the role of ground high-precision magnetic survey in the exploration of pegmatite spodumene deposits is often overlooked. In order to study the applicability of ground high-precision magnetic survey in finding hidden ore bodies, this paper takes the Jiajika mining area as an example and selects representative rock samples in the mining area for magnetic parameter measurement. The study shows that the magnetism of rocks and ores in the Jiajika mining area is weak overall, but there are high magnetic susceptibility and residual magnetization intensity in local areas. The 1: 50, 000 geomagnetic anomaly characteristics show that there are a series of medium-strong positive or negative anomalies in the Jiajika dome area, which are related to pegmatite veins. The 1: 5000 magnetic survey profile data further confirms that these anomalies are mainly caused by deep underground geological factors. Comprehensive analysis shows that the geomagnetic field characteristics of the Jiajika mining area are significantly different from those outside the dome area. Ground high-precision magnetic survey plays an important role in the exploration of pegmatite spodumene deposits. Its application potential cannot be ignored because spodumene deposits are non-magnetic. It also has certain reference significance for the prospecting of similar deposits.

       

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