Abstract
Gold was mainly concentrated in the Earth's solid and compacted Fe–Ni core during the planet’s accretionary stage, along with other highly siderophile elements. During partial melting of the mantle, gold is derived from the magmatic fluids that circulated to the surface in various tectonic contexts (cratons, ocean basins, divergent margins, convergent basins, and transform boundaries). Tectonic models and related geological processes control the genesis of ores not only of gold but of other metal deposits in Earth's geology and history, including the opening and closing of ocean basins, orogenesis of mountain ranges and geological structures, the distribution of mineral resources, and paleoclimates.
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Further Readings
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Macdonald EH (ed) (2007) Geology of gold ore deposits. In: Handbook of gold exploration and evaluation. Woodhead Publishing, pp 62–133
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Sanz J, Tomasa O (2017) Elements i Recursos minerals: aplicacions i reciclatge. Manresa, Catalonia. Zenobita Edicions/Iniciativa Digital Politècnica (Catalan 3rd digital edition). http://hdl.handle.net/2117/105113
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USGS (2021) Commodity statistics and information. Gold. URL: https://www.usgs.gov/centers/nmic/gold-statistics-and-information. Last accessed May 2021
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Sanz, J., Tomasa, O., Jimenez-Franco, A., Sidki-Rius, N. (2022). Gold (Au) [Z = 79]. In: Elements and Mineral Resources. Springer Textbooks in Earth Sciences, Geography and Environment. Springer, Cham. https://doi.org/10.1007/978-3-030-85889-6_23
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DOI: https://doi.org/10.1007/978-3-030-85889-6_23
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