CSAMT法在巴音戈壁盆地构造单元和砂体识别中的应用

    Application of CSAMT method in identifying structural units and sand bodies in the Bayingobi Basin

    • 摘要: 巴音戈壁盆地乌力吉地区铀成矿条件优越,但第四系覆盖广泛,构造单元和目标层砂体展布特征不明,且目前地质图比例尺过小,研究区构造单元的展布尚不明确,难以满足铀矿勘查需求。通过开展可控源音频大地电磁测量(CSAMT),获得了沉积盖层的电性结构,推断了目标层砂体的空间展布特征,主要分布于乌力吉凹陷和托莱凹陷内,埋深60~330 m,厚50~340 m。对研究区构造单元进行了新的划分,为“两凹夹一凸”的构造格架,断裂控制了构造单元边界。通过实地地质调查及后续钻孔的验证,证明了本次解释结果的准确性,为相关地区的砂岩型铀矿勘查提供了参考与借鉴。

       

      Abstract: The Uliji Area of the Bayingobi Basin has superior uranium mineralization conditions, but the Quaternary System covers a wide range, and the distribution characteristics of structural units and target sand bodies are unclear. Moreover, the scale of the geological map is currently too small, and the distribution of structural units in the study area is not yet clear, making it difficult to meet the needs of uranium exploration. By conducting controllable source audio magnetotelluric surveys(CSAMT), the electrical structure of the sedimentary cover layer is obtained, and the spatial distribution characteristics of the target sand body are inferred, mainly distributed in the Uliji and Tolai Depressions, with a burial depth of 60-330 m and a thickness of 50-340 m. A new division has been made for the structural units in the research area, which is a structural framework of “two depressions sandwiched with a convex”, with faults controlling the boundaries of the structural units. Through on-site geological surveys and subsequent drilling verification, the accuracy of the interpretation results has been proven, providing reference for the exploration of sandstone type uranium deposits in relevant regions.

       

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