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Assessment of Geochemical Anomaly Uncertainty Through Geostatistical Simulation and Singularity Analysis

机译:通过地质统计模拟和奇异性分析评估地球化学异常不确定性

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摘要

Geochemical anomalies are commonly separated into different geochemical anomaly levels based on one or more thresholds. However, this practice may cause some important geochemical anomaly information to be lost and subsequently draw wrong decisions for mineral exploration. In addition, previous studies indicate that sparse geochemical sampling always entails uncertainty resulting from conventional geochemical interpolation methods because of smoothing effect. Uncertainty can propagate through the various steps of geochemical data analysis that may lead to significant impact on the final results (e.g., anomaly interpretation and mineral exploration). For geochemical anomaly identification, quantifying the probability of unsampled locations and characterizing the spatial uncertainty of geochemical anomaly based on (not) exceeding a key threshold is very important for practical demands such as exploration risk assessment. Considering the limitations of deterministic modeling method and geochemical anomaly assessment, this study proposes a new method of geochemical anomaly uncertainty assessment by combining geostatistical simulation and singularity analysis. A case study for Au anomaly uncertainty assessment is presented in the west Tianshan region (China) so as to verify the feasibility and effectiveness of the proposed method. The sequential Gaussian simulation was adopted to generate a set of equiprobable realizations that were subsequently employed to produce a series of corresponding singularity index realizations by means of singularity analysis. Critical thresholds of E-type singularity index () were determined by the method of singularity-quantile plot analysis, which were used to simulate the spatial uncertainty of Au anomaly in the study area. The results show that the risk probability of Au anomaly characterized by (not) exceedance of a critical threshold can be considered as an important reference for exploration decision-making and risk management.
机译:基于一个或多个阈值,地球化学异常通常分为不同的地球化学异常水平。然而,这种做法可能导致一些重要的地球化学异常信息丢失,随后为矿物勘探制定了错误的决定。此外,以前的研究表明,由于平滑效果,稀疏地球化学抽样总是需要由传统地球化学插值方法产生的不确定性。不确定性可以通过地球化学数据分析的各个步骤繁殖,这可能导致对最终结果的重大影响(例如,异常解释和矿物勘探)。对于地球化学异常鉴定,量化未采样的位置并基于(不)超过关键阈值的地球化学异常的空间不确定性对实际要求进行了非常重要的,这对于勘探风险评估等实际需求非常重要。考虑到确定性建模方法和地球化学异常评估的局限性,本研究提出了通过结合地统计模拟和奇异性分析来提出一种新的地球化学异常不确定性评估方法。西天山地区(中国)介绍了Au异常不确定性评估的案例研究,以验证拟议方法的可行性和有效性。采用顺序高斯模拟来产生一组替代的实现,随后采用奇异性分析产生一系列相应的奇点指数实现。通过奇异性 - 定量绘图分析方法确定e型奇点指数()的临界阈值,该曲线分析方法用于模拟研究区域中Au异常的空间不确定性。结果表明,Au异常的风险概率(不是)超越关键阈值的表征可以被视为勘探决策和风险管理的重要参考。

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