Mathematical, Physical, and Chemical Interpretations of Structural Control and Contributions to Gold Mineralization
Authors: Yin Jian Zhao , Li Kuinuan , Shi Hongyun , Yin Haoyu , Chao Yuhong 
Published: January 2025

Using the gold provinces in the northern margin of the North China Platform and the western Canadian orogenic belt—separated by thousands of miles—as examples, this article examines the temporal and spatial relationship between global gold deposits and geological structures; that is, gold metallogenic series within a region often correspond to the fault structural systems in that area. Fault structures at different hierarchical levels within the same fault system play distinct roles in gold deposit formation: the first-level deep and large faults are often the channels for the rise of rock-forming materials and their carriers, and control countless gold belts and/or gold fields on the earth&#039;s surface. The secondary fault system controls gold fields and/or gold deposits of different sizes. The third-level fault controls the gold ore body of a specific deposit. The mechanical properties of faults, their activity periods, and the development of structural rocks influence the timing and stages of mineralization, as well as the intensity and structure/texture of the resulting ore deposits. Post-ore-forming structures play a crucial role in converting primary gold deposits into placer gold deposits through processes such as uplift, displacement, transformation, and destruction of the original deposits. The deep-seated mechanisms underlying the structural control of gold mineralization align with principles of mathematics, physics, and chemistry. Nonlinear coherent effects within the far-from-equilibrium dissipative structures of fold-fault-ore-forming systems are significant. The localized dissipative structures resulting from tectonic and/or structural activity drive the final stages of gold mineralization. The essence of mineralization is the result of steady-state instability developing into a dissipative structure far away from equilibrium. The structures facilitate the conduction, extraction, further enrichment, and upward intrusion of deep ore-bearing fluids through special physical effects like seismic pumping, expansion, and re-fracture of mineralized zones. Deep and large faults also contribute to the formation of gold belts, ore fields, and deposits by inducing localized melting of rocks at different depths and mixing within the same tectonic system, as well as certain mutations in the ore-forming fluid entering the nonlinear low-pressure expansion zone, which causes hydrothermal boiling and a rapid nonlinear decrease in the solubility of the ore fluid. From a chemical perspective, the low-pressure expansion spaces formed by these structures act as vast mineralization reactors, in which rock-forming and mineralizing materials from different sources undergo violent physical and chemical reactions. This melting reactor not only greatly changes the temperature and pressure of the fluid, but also leads to drastic changes in many chemical conditions such as oxygen fugacity, pH, and electrolyte balance, thus creating conditions for the formation of gold deposits. Some structures, such as epigenetic faults, intersect and divide each other to create differences in the bottom topography, hydrodynamics, hydrogeochemistry, and physical chemistry in the basin. These variations create favorable space for the accumulation of large quantities of minerals, contributing to the formation of large or even super-large gold deposits.