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    松辽盆地乾安地区四方台组砂岩型渗入−渗出耦合铀成矿模式与找矿方向

    Exudation−infiltration coupled mineralization model and prospecting direction of sandstone−type uranium deposit in Sifangtai Formation, Qian'an area, Songliao Basin

    • 摘要:
      研究目的 松辽盆地中部腹地乾安地区四方台组砂岩型铀成矿条件与成矿模式研究相对薄弱。全面梳理该地区砂岩型铀矿的成矿条件、综合评价其成矿潜力进而明确其找矿方向,可为松辽盆地的铀矿勘查工作开辟新方向。
      研究方法 本文通过岩心、测井、地震、微量元素等数据的综合分析,在构造、建造和改造特征研究基础上,系统总结乾安地区四方台组砂岩型铀矿的成矿要素。
      研究结果 乾安地区四方台组具备构造天窗、深大断裂、辫状河三角洲河道砂体、良好地层铀源条件与后生改造等基本成矿条件。在此基础上首次从渗入、渗出两个角度对乾安地区四方台组的铀成矿条件分别进行了系统梳理,认为四方台组同时具备渗入和渗出两种铀成矿条件,且渗出成矿占优。基于此构建了乾安地区四方台组渗出−渗入耦合铀成矿模式,认为浅部渗入流体和深部渗出流体的交汇部位是有利成矿区,提出让字镇—查干花一带四方台组的辫状河−辫状河平原河道砂体具有较大的资源潜力,可作为盆地腹部铀矿勘查的优先探索方向。
      结论 本研究首次将渗出成矿思路引入到松辽盆地四方台组红杂色建造铀成矿条件的系统评价,改变了以往渗入角度评价目标层的单一思路,可有效拓展盆地腹地红杂色层的找矿思路,进而拓展铀矿的找矿空间。

       

      Abstract:
      This paper is the result of mineral exploration engineering.
      Objective The study of uranium metallogenic conditions and mineralization model of Sifangtai Formation, Qian’an area in the hinterland of Songliao basin is relatively weak. Comprehensively analyzing the mineralization conditions of the sandstone-type uranium deposits, evaluating their mineralization potential, and clarifying their exploration directions can develop new direction for uranium exploration in the Songliao Basin.
      Methods Through comprehensive analysis of core, logging, seismic, trace element and other data, the tectonics, stratigraphy and transformation of Sifangtai Formation in Qian’an area has been sorted, and it is the first time to systematically summarize the uranium metallogenic elements of sandstone-type uranium deposits in the the hinterland of Songliao Basin.
      Results Sifangtai Formation in Qian'an area has favorable metallogenic conditions such as structural window, deep and large faults, braided river delta channel sand belts, good uranium source conditions and epigenetic transformation. It is considered that Sifangtai Formation infiltrative and exudative uranium metallogenic conditions, and exudative metallogeny is dominant. Based on these facts, the exudation-infiltration coupled uranium metallogenic model of Sifangtai Formation, Qian'an area, Centrel Songliao Basin, has been constructed. Finally, it is proposed that the braided river to braided river plain channel sand in Rangzhi–Chaganhua Town has great uranium metallogenic potential, which has been predicted to be the most favorable object for further exploration.
      Conclusions This study is the first to introduce exudative metallogeny into the systematic evaluation of uranium mineralization conditions in Sifangtai Formations of the Songliao Basin, changing the previous single approach of evaluating the target layer from the perspective of infiltration metallogeny. It can effectively expand the exploration thinking of the red variegated formations in the hinterland of the basin, thereby greatly expanding the prospecting range in the Songliao Basin.

       

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