Thermodynamic Model Unveils Gold's Journey to Earth's Surface

Researchers have used a thermodynamic model to explain how gold deposits are formed in volcanic settings. The model reveals the crucial role of a previously unconfirmed gold-trisulfur complex (Au-S3). Under specific mantle pressures and temperatures, this complex efficiently transfers gold from the mantle into magma, ultimately leading to its surfacing through volcanic activity. This finding explains the high gold concentrations in certain subduction zone ore deposits and has significant implications for gold exploration.