Implication of multifractal analysis for quantitative evaluation of mineral resources in the Central Kunlun area, Xinjiang, China

Author:

Zhang Yuepeng1,Ye Xiaofeng2,Xie Shuyun1ORCID,Zhou Xiaoying2,Awadelseid Salah Fadlallah3,Yaisamut Oraphan14,Meng Fanxing1

Affiliation:

1. State Key Laboratory of Geological Processes and Mineral Resources (GPMR), Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

2. Geophysical and Geochemical Prospecting Group, Geological and Mineral Exploration and Development Bureau, Changji, Xinjiang 831100, China

3. Department of Mineral Resources, College of Petroleum Geology and Minerals, University of Bahri, Khartoum, Sudan

4. Geotechnology Division, Department of Mineral Resources, Ministry of Natural Resources and Environment, 75/10 Rama VI Road, Ratchathewi, Bangkok 10400, Thailand

Abstract

Extensive research has been conducted to evaluate mineral resource potential based on geochemical data, but this work is still challenging due to the existence of multiple evaluation solutions based on different methods. In this paper, we combine the multifractal analysis method with typical multivariate statistical methods to analyse the spatial characteristics of geochemical stream sediment data, aiming to quantitatively study the ore-forming potential of the elements in the Central Kunlun area of Xinjiang, China. An R -type cluster analysis, Pearson correlation analysis, and principal component analysis are used to explore the correlations among the 12 target elements. The multifractal model is constructed using the method of moments to analyse the spatial distribution patterns of the elements, and corresponding multifractal parameters are extracted to quantitatively describe their ore-forming strengths in the study area. The results show that Co, V, Ti, Fe 2 O 3 , MgO and Cu compose a group of elements closely related to the regional geological background, while Pb, Zn, Bi, Sn, Au and Ba are potential metallogenic elements with relatively high ore-forming strengths and favourable ore-forming potential. Multifractal theory further validates and evaluates the favourable ore-forming element group obtained through conventional geochemical multivariate statistical methods, thus providing a new idea for small-scale geochemical prospecting. 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

Natural Science Foundation of China

National Natural Science Key Fund Project

Northwestern Basic Geological Survey and Data Update Project of China Geological Survey

Natural Science Key Project of Inner Mongolia Education Department

Inner Mongolia Natural Science Foundation

Publisher

Geological Society of London

Subject

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

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