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Non-Linear Theory and Power-Law Models for Information Integration and Mineral Resources Quantitative Assessments

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Abstract

Singular physical or chemical processes may result in anomalous amounts of energy release or mass accumulation that, generally, are confined to narrow intervals in space or time. Singularity is a property of different types of non-linear natural processes including cloud formation, rainfall, hurricanes, flooding, landslides, earthquakes, wildfires, and mineralization. The end products of these non-linear processes can be modeled as fractals or multifractals. Hydrothermal processes in the Earth’s crust can result in ore deposits characterized by high concentrations of metals with fractal or multifractal properties. Here we show that the non-linear properties of the end products of singular mineralization processes can be applied for prediction of undiscovered mineral deposits and for quantitative mineral resource assessment, whether for mineral exploration or for regional, national and global planning for mineral resource utilization. In addition to the general theory and framework for the non-linear mineral resources assessment, this paper focuses on several power-law models proposed for characterizing non-linear properties of mineralization and for geoinformation extraction and integration. The theories, methods, and computer system discussed in this paper were validated using a case study dealing with hydrothermal Au mineral potential in southern Nova Scotia, Canada.

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Authors and Affiliations

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

    Qiuming Cheng

  2. Department of Earth and Space Science and Engineering, York University, Toronto, M3J1P3, Canada

    Qiuming Cheng

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  1. Qiuming Cheng
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Cheng, Q. Non-Linear Theory and Power-Law Models for Information Integration and Mineral Resources Quantitative Assessments. Math Geosci 40, 503–532 (2008). https://doi.org/10.1007/s11004-008-9172-6

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  • DOI: https://doi.org/10.1007/s11004-008-9172-6

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