Abstract

Abstract. This contribution introduces a fractal filtering technique newly developed on the basis of a spectral energy density vs. area power-law model in the context of multifractal theory. It can be used to map anisotropic singularities of geochemical landscapes created from geochemical concentration values in various surface media such as soils, stream sediments, tills and water. A geochemical landscape can be converted into a Fourier domain in which the spectral energy density is plotted against the area (in wave number units), and the relationship between the spectrum energy density (S) and the area (A) enclosed by the above-threshold spectrum energy density can be fitted by power-law models. Mixed geochemical landscape patterns can be fitted with different S-A power-law models in the frequency domain. Fractal filters can be defined according to these different S-A models and used to decompose the geochemical patterns into components with different self-similarities. The fractal filtering method was applied to a geochemical dataset from 7,349 stream sediment samples collected from Gejiu mineral district, which is famous for its word-class tin and copper production. Anomalies in three different scales were decomposed from total values of the trace elements As, Sn, Cu, Zn, Pb, and Cd. These anomalies generally correspond to various geological features and geological processes such as sedimentary rocks, intrusions, fault intersections and mineralization.

Highlights

  • Toxic elements such as arsenic occur naturally in surface media such as soils, water, and sediments, in part because of the weathering of rocks and ores that contain elevated concentrations of ore and toxic elements

  • A different model was proposed on the basis of extreme value distributions of 2-D multifractal fields stating that the concentration value (C) and the area enclosed by the cutoff concentration value (A[> C]) follow a power-law relation (Cheng et al, 1994)

  • A generalized self-similarity spectrum-area model (S-A) model was successfully used to decompose the mixed geochemical landscapes caused by various scales of geological processes and features

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Summary

Introduction

Toxic elements such as arsenic occur naturally in surface media such as soils, water, and sediments, in part because of the weathering of rocks and ores that contain elevated concentrations of ore and toxic elements. There are many types of hydrothermal deposits that contain minerals such as arsenopyrite with high levels of arsenic and other toxic elements, including gold deposits, Sn deposits and Pb/Zn deposits. Due to high concentrations of these elements in ores and country rocks, secondary weathering processes and human activities such as mining can cause dispersion of these elements in surface media. Arsenic contamination related to mining and geology has been actively studied in China.

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