Abstract

The spatial distribution of elements can be regarded as a numerical field of concentration values with a continuous spatial coverage. An active area of research is to discover geologically meaningful relationships among elements from their spatial distribution. To solve this problem, we proposed an association rule mining method based on clustered events of spatial autocorrelation and applied it to the polymetallic deposits of the Chahanwusu River area, Qinghai Province, China. The elemental data for stream sediments were first clustered into HH (high–high), LL (low–low), HL (high–low), and LH (low–high) groups by using local Moran’s I clustering map (LMIC). Then, the Apriori algorithm was used to mine the association rules among different elements in these clusters. More than 86% of the mined rule points are located within 1000 m of faults and near known ore occurrences and occur in the upper reaches of the stream and catchment areas. In addition, we found that the Middle Triassic granodiorite is enriched in sulfophile elements, e.g., Zn, Ag, and Cd, and the Early Permian granite quartz diorite (P1γδο) coexists with Cu and associated elements. Therefore, the proposed algorithm is an effective method for mining coexistence patterns of elements and provides an insight into their enrichment mechanisms.

Highlights

  • Spatial autocorrelation analysis focuses on the similarity of attributes, as well as spatial similarity between one geological entity and adjacent entities

  • We propose an association rule mining method to study the cross correlation of concentration fields based on clustered events of spatial autocorrelation

  • Geary’s C and local Getis–Ord’s G, local Moran’s I can identify points of HH, LL, LH, and HL clustering with a precise meaning for each category, which makes it a better local autocorrelation indicator for association rule mining

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Summary

Introduction

Spatial autocorrelation analysis focuses on the similarity of attributes, as well as spatial similarity between one geological entity and adjacent entities. The spatial distribution of concentrations of elements can be regarded as a numerical field with a continued spatial coverage, which can be characterized by using spatial autocorrelation among different elements. Korobova and Romanov (2009) stressed that the nonrandom characteristics and spatial structure of geochemical data depend on the concentration field [1]. Analysis of the concentration field includes comparison of samples to recognize anomalies and using the spatial correlation among elements to explain geochemical processes. It is necessary to consider spatial auto- and cross correlation in geochemical studies. It is of great significance to study the distribution, enrichment, and relationships among different elements to understand regional magmatism and oreforming process [2]

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