Metal Transport and Deposition in Ore-Forming Hydrothermal Fluids

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".

Deadline for manuscript submissions: closed (1 September 2022) | Viewed by 1176

Special Issue Editors

Earth and Environmental Division, Los Alamos National Laboratory, Los Alamos, NM 87545, USA
Interests: hydrothermal fluid; aqueous chemistry; thermodynamics
1. New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801, USA
2. Department of Earth & Environmental Sciences, New Mexico Institute of Mining and Technology, Socorro, NM 87801, USA
Interests: critical minerals; ore deposits; pegmatites; thermodynamic modeling; fluid–rock interaction; mineralogy
Commonwealth Scientific & Industrial Research Organisation (CSIRO), Clayton, VIC 3168, Australia
Interests: hydrothermal experiment; thermodynamic modeling; fluid–mineral interactions; ore deposits; mineral processing; critical minerals

Special Issue Information

Dear Colleagues,

Hydrothermal fluids control large-scale transport, distribution, and concentration of metals in the Earth’s crust. Evidence for these processes can be found in active geothermal systems and also in deeper fossil systems from the study of veins, fluid inclusions, and alteration mineralogy in ore deposits and metasomatized rocks. Our ability to predict metal concentration and ore formation during the evolution of magmatic–hydrothermal systems depends on our knowledge of the physicochemical properties and the speciation of elements in these fluids, the effects of fluid–rock interaction, and other processes such as boiling and fluid mixing. We invite contributions aimed at evaluating the role of hydrothermal fluids on the behavior of metals in various geological processes (e.g., ore formation and geothermal systems). We envisage this Special Issue covering a range of topics and approaches, starting with geological evidence (alteration mineralogy, fluid inclusions, etc.) and geochemical modeling of fluid-driven processes in natural systems and continuing with fundamental experimental and theoretical research on metal speciation, partitioning, and precipitation processes. We encourage contributions that evaluate the chemistry of these fluids and hydrothermal minerals at elevated temperature and pressure, the partitioning of elements among phases, and the properties of solvents and solutes commonly occurring in nature. We also invite contributions aimed at using geochemical and molecular modeling to predict the chemical properties of fluids and solutes, incorporation of metals and solubility of minerals, their structures, and the nature of solute–solvent interactions at an elevated temperature. Through the integration of these topics, we aim to shed new light on frontier research on fluid-mediated processes that control the mobility of elements and ore deposition in the Earth’s crust.

Dr. Artaches (Artas) Migdisov
Dr. Alexander Gysi
Dr. Weihua Liu
Guest Editors

Manuscript Submission Information

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  • hydrothermal systems
  • transport, concentration, fractionation
  • aqueous speciation
  • thermodynamic modeling
  • critical minerals
  • molecular dynamics
  • hydrothermal experiments
  • metal complexation
  • ore deposits
  • fluid inclusions
  • ore mineralogy
  • geothermal

Published Papers

There is no accepted submissions to this special issue at this moment.
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