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July 3, 2025

Geological mystery: Study unearths how copper deposits formed

Evolution of magmatic redox from oceanic subduction to continental collision. Credit: Science Advances (2025). DOI: 10.1126/sciadv.adx4474
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Evolution of magmatic redox from oceanic subduction to continental collision. Credit: Science Advances (2025). DOI: 10.1126/sciadv.adx4474

An international study has revealed how continental collisions may have supercharged the Earth's richest deposits of copper, a metal critical for clean energy technologies and global infrastructure.

Dr. Yongjun Lu, from The University of Western Australia's School of Earth and Oceans and a principal geoscientist at RSC, was co-author of the study published in .

Researchers analyzed magmatic rocks from the Gangdese belt in southern Tibet鈥攐ne of the world's richest porphyry copper provinces.

Porphyry copper deposits are the largest copper source globally and form when hot hydrothermal fluids travel through fractured rocks and precipitate copper minerals.

"The deposits are typically associated with magmas formed above active subduction zones, where oxidized fluids from descending enrich the overlying mantle," Dr. Lu said.

"Yet, some of the largest copper deposits鈥攍ike those in southern Tibet鈥攆ormed millions of years after subduction had ceased, which has been puzzling scientists for decades."

Researchers found sediments from the Indian plate鈥攔ich in oxidized components such as carbonates and sulfates鈥攚ere recycled deep into the mantle during continental collision. These materials helped generate oxidized magmas ideal for concentrating copper.

Using mercury and magnesium isotope analyses alongside geochemical fingerprinting, the team identified evidence of oxidized sedimentary material contributing to post-collisional magmas.

"This finding challenges the notion that only oceanic subduction introduces such oxidants into the mantle," Dr. Lu said.

"Think of it as a second wind for copper-forming magmas鈥攅ven after the oceanic plate is gone, recycled crustal sediments can continue to fuel metal-rich systems for millions of years."

The results will help to expand the search for future resources into tectonic regions previously overlooked.

"It changes the way we think about where and how to look for giant copper deposits and highlights the potential of post-subduction settings鈥攑articularly those involving continent-continent collision鈥攁s important frontiers for exploration," Dr. Lu said.

"The discovery is timely, as the global demand for has increased with the transition to renewable energy and electrified economies."

The research was conducted in collaboration with partners from institutions in China and Europe.

More information: Zhiming Yang et al, Oxidized sediment recycling as a driver for postsubduction porphyry copper formation, Science Advances (2025).

Journal information: Science Advances

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Analysis of magmatic rocks from southern Tibet indicates that continental collisions can recycle oxidized sediments deep into the mantle, generating oxidized magmas favorable for copper concentration even after subduction ends. This process expands the potential for copper deposit formation beyond traditional subduction zones, informing future exploration strategies.

This summary was automatically generated using LLM.