Analysis of geochemical patterns in a soil profile over mineralized bedrock

Author:

Yang Jie12ORCID,Yuan Zhaoxian3,Grunsky Eric4,Cheng Qiuming1,Zhou Shubin5

Affiliation:

1. State Key Lab of Geological Processes and Mineral Resources, China University of Geosciences (Beijing), Beijing, China

2. Institute of Earth Sciences, China University of Geosciences (Beijing), Beijing, China

3. Institute of Resource and Environmental Engineering, Hebei Geo University, Shijiazhuang, China

4. School of Earth and Environmental Sciences, University of Waterloo, Waterloo, Canada

5. Department of Earth and Environmental Sciences, Faculty of Science and Engineering, Macquarie University, Sydney, Australia

Abstract

Transported soils cause difficulties in the identification of geochemical anomalies. It has been demonstrated that the joint application of local singularity analysis (LSA) and principal component analysis (PCA) can identify geochemical anomalies effectively, especially in regolith-covered areas. However, more convincing evidence is needed to explain the reasons for this. In this study, a soil profile overlying several mineralized veins cutting through bedrock was analysed in situ using a portable X-ray fluorescence spectrometer. The patterns of two mineralization-related elements, Cu and Mo, were analysed. The results revealed that the element concentrations of the soil sharply decreased as the distance from the bedrock increased, and this relationship can be described by a power-law model. LSA enhanced several vein-like anomalies corresponding to the mineralization veins in the bedrock, and the presence of vertically elongated weak anomalies in the soil indicates the migration of ore elements originating from the underlying bedrock through the soil. The statistics show that the patterns of the local singularity index (LSI) are stable at different depths and in different media, whereas the concentration patterns are not. In addition, the mineralization-related elements have a higher correlation coefficient for the LSI than for the concentration. Since a previous simulation study determined that a mineralization-indicative first principal component prefers that the variables have a close relationship and that the variables have similar patterns in different geological objects, the patterns discovered in this study explain why LSA is effective in identifying geochemical anomalies, especially when combined with PCA. Supplementary material: the high-resolution photo, the element concentration data and the lithologic data of the profile are available at https://doi.org/10.6084/m9.figshare.c.5957122 Thematic collection: This article is part of the Applications of Innovations in Geochemical Data Analysis collection available at: https://www.lyellcollection.org/cc/applications-of-innovations-in-geochemical-data-analysis

Funder

Ministry of Science and Technology of the People's Republic of China

National Natural Science Foundation of China

Publisher

Geological Society of London

Subject

General Earth and Planetary Sciences,Geochemistry and Petrology,General Environmental Science,General Chemistry

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