全球钾盐经典成矿模式及其地球物理勘探方法的研究现状与展望

Global representative metallogenic models and geophysical exploration methods of sylvite: Current research status and prospects

  • 摘要:
    背景 钾盐是保障粮食安全和农业可持续发展的重要战略性矿产资源,全球约90%的钾盐用于生产钾肥。我国等发展中国家长期面临对外依存度高、资源接续不足的挑战,这种供需格局要求我国必须加速探索成矿规律与勘探技术创新,以突破资源瓶颈。
    目的 系统总结了全球钾盐成矿模式,探索深部及构造复杂区钾盐资源勘查思路,为提高钾盐勘查效率提供理论支撑。
    方法 围绕海相与陆相环境下的成钾地质背景与成钾条件,从构造活动、蒸发环境、卤水来源等关键因素出发,分析富钾机制。同时,梳理了当前钾盐地球物理勘探方法的研究现状与应用进展,具体展示了重力、电磁法、地震、测井等地球物理技术在钾盐资源勘探中的应用效果。
    结果和结论 (1)钾盐成矿模式揭示了气候−构造−物源等多因素的耦合作用。(2)重力勘探利用密度差异识别盐丘构造;电磁法对高矿化度卤水敏感;地震勘探借助叠前深度偏移技术,可以实现盐层空间形态的精细刻画。(3)深部隐伏矿体受构造变形屏蔽,地震信号衰减严重;电磁法在低阻覆盖区垂向分辨率不足;浅层重力勘探易受地形干扰等问题仍制约着勘探精度与深度。通过多学科融合、智能化勘探技术的应用以及钾盐成矿模式的深入研究,钾盐资源的勘查与开发将更加精准和高效,为全球复杂盆地的资源评价突破提供理论依据,为深部钾盐勘探提供创新解决方案。

     

    Abstract:
    Background Sylvite serves as a strategic mineral resource that plays a significant role in ensuring food safety and sustainable agricultural development, with approximately 90% of global potash resources used for potassium fertilizer production. However, developing countries such as China have long faced the challenges of heavy dependence on potash imports and insufficient potash resource continuity. Such a supply and demand framework causes China to speed up research on potash metallogenic patterns and technical innovations in potash exploration. This will help overcome resource bottlenecks.
    Objective This study presented a systematic summary of global potash metallogenic models and investigated the approaches of potash exploration in deep and structurally complex areas, aiming to provide theoretical support for improving potash exploration efficiency.
    Methods Focusing on the geological settings and conditions of potash mineralization in marine and continental environments, the study analyzed potash enrichment mechanisms from the perspective of key factors, including tectonic activity, evaporation environments, and brine sources. hhFurthermore, this study reviewed the current research status and application progress in the geophysical exploration methods of potash, specifically exhibiting the application effects of geophysical technologies such as gravity, electromagnetic, seismic, and logging methods in potash exploration.
    Results and Conclusions Sylvite metallogenic models reflect the coupling effects of multiple factors, including climate, structures, and provenance. Gravity exploration identifies salt dome structures based on density differences. In contrast, electromagnetic methods are sensitive to high-salinity brines, while seismic methods allow for fine-scale characterization of the spatial morphology of potash layers when combined with pre-stack depth migration technology. However, deep concealed ore bodies are shielded by structural deformations, leading to significant attenuation of seismic signals. Furthermore, electromagnetic methods suffer from insufficient vertical resolution in low-resistance areas, while shallow gravity exploration is prone to terrain interference. These challenges still limit the precision and depth of potash exploration. Nevertheless, multidisciplinary integration, the application of intelligent exploration technologies, and in-depth research on potash metallogenic models will contribute to more accurate and efficient exploration and development of potash resources. This provides theoretical bases for breakthroughs in the evaluation of potash resources in global complex basins and offers innovative solutions for deep potash exploration.

     

/

返回文章
返回