Research news on hydrothermal processes

Hydrothermal processes are geochemical and geological phenomena driven by the circulation of heated aqueous fluids within the Earth’s crust, typically associated with magmatic intrusions, mid-ocean ridges, and sedimentary basins. These fluids, often saline and metal-bearing, interact with surrounding rocks, causing mineral dissolution, transport, and precipitation, which leads to metasomatism, alteration halos, and the formation of hydrothermal ore deposits (e.g., sulfides, quartz veins). Thermodynamic and kinetic controls, including temperature, pressure, fluid composition, and redox conditions, govern mineral stability and reaction pathways. Hydrothermal systems are key to understanding crustal heat and mass transfer, fluid–rock interaction, and elemental cycling in lithospheric environments.

Ahuachapán and its restive neighbors

From a geothermal hotspot to the one-time "Lighthouse of the Pacific," the heat is on beneath the volcanic landscape of western El Salvador.

Why subduction zones act as the Earth's 'gold kitchens'

Earth's "gold kitchen" lies deep beneath the seafloor. Island arcs, whose volcanoes form above subduction zones where one oceanic plate sinks beneath another, are often particularly rich in gold. The reasons for this have ...

Hydrothermal plumes as invisible transport pathways for iron

A new review led by the MARUM—Center for Marine Environmental Sciences at the University of Bremen—highlights how hydrothermal vents on the seafloor shape iron availability and influence the global oceanic element cycles. ...

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