Structural and non-structural statistical methods: implications for delineating geochemical anomalies

B. Roshanravan, S. H. Tabatabaei, O. Kreuzer, Hamid Moini, M. Parsa
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引用次数: 16

Abstract

ABSTRACT Geochemical sampling media, be they rock chip, soil or stream sediment samples, routinely collected in mineral exploration, are key to detecting mineralisation-related geochemical dispersion patterns. Notwithstanding the diversity of methods applied to geochemical anomaly detection, they can be broadly divided into two major groups, namely structural and non-structural techniques. The former group covers those methods in which threshold values are assigned based on sample location while the sample locations are not required in the application of the non-structural techniques. In this study, rock chip samples from the Shadan porphyry copper–gold deposit are used to address the question as to how structural and non-structural methods can separate geochemical populations for the purpose of a deposit-scale study. It was revealed that the two structural techniques used in this study, concentration-area (C-A) fractal and U-spatial statistic methods, outperformed the non-structural techniques employed in this study.
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构造和非构造统计方法:圈定地球化学异常的意义
地球化学取样介质,无论是岩屑、土壤还是水系沉积物样品,都是矿产勘查过程中常规采集的地球化学弥散模式的关键。尽管地球化学异常检测的方法多种多样,但它们大致可分为两大类,即构造技术和非构造技术。前一组涵盖了基于样本位置分配阈值的方法,而在非结构技术的应用中不需要样本位置。本研究利用沙丹斑岩型铜金矿床的岩屑样品,探讨构造和非构造方法如何区分地球化学种群,以进行矿床尺度研究。结果表明,本研究中使用的两种结构方法,即浓度-面积(C-A)分形和u -空间统计方法,优于本研究中使用的非结构方法。
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CiteScore
1.70
自引率
10.00%
发文量
17
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