Regional to nanoscale ore deposit metallogeny
- José María González Jiménez (Instituto Andaluz de Ciencias de la Tierra & Geosciences CSIC-Hub)
- Tuesday, September 10 | 12:00 h CET
- Online (YouTube link) & GEO3BCN-CSIC’s conference room.
This seminar is organized by Geosciences Barcelona & the Faculty of Earth Sciences of the University of Barcelona in collaboration with the Geosciences CSIC-Hub.
Abstract
The potential endowment of metals in continental crust is enormous, with a large proportion of their resources confined in a variety of ore deposits hosted in either (peri)-cratonic and convergent margins, clustered in either provinces or metallogenic belts. In these settings, several types of ore deposits enriched in precious metals, with a wide range of sizes, usually develop in different restricted epochs. It is currently debated whether a given metal deposits has a unique mode of formation, or it represent a case within a spectrum of mineralization style, formed by an optimum convergence of common geological processes. The traditional notion of metal endowment in a given metallogenic province is that metal accumulated by highly efficient magmatic-hydrothermal enrichment processes operating in a chemically “average” crust. However, many recent frontline studies suggest that metal endowment requires the possible existence of anomalously enriched sources and/or magmas. It is now under debate whether these metal-rich reservoirs exist in the mantle, the mantle-crust transition or the crust. In this scenario, our research efforts must be tailored to determine the fundamental regional to nanoscale factors that control metal transfer from a deep mantle or lower crustal source to the shallow crust where the ore deposits accessible to mining are found. In this communication I will provide key evidence about how metals are transferred from the lower shallowest domains of the continental lithosphere where metal-rich magmas parental of magmatic-hydrothermal deposits are formed. This unprecedented information on the source, distribution and enrichment mechanisms of metals is a valuable tools allowing more efficient exploration and beneficiation metals.