Ancient ocean floors could help search for critical minerals

Publicly released:
Australia; QLD
Examining ocean floors key to minerals needed for renewable energy. Image: Supplied
Examining ocean floors key to minerals needed for renewable energy. Image: Supplied

Studying ancient ocean floors could help discover minerals needed to produce electric cars and solar panels, according to Australian experts.

Media release

From: The University of Queensland

Studying ancient ocean floors could help discover minerals needed to produce electric cars and solar panels.

Researchers at The University of Queensland led a collaborative study that examined the remnants of ocean floors in eastern Australia and central Asia and applied a method to date the age of calcite trapped inside.

Dr Renjie Zhou from UQ’s School of Earth and Environmental Sciences said the findings could make it easier to source critical minerals used in renewable and clean technologies.

“Calcite and other hydrothermal minerals are often observed in critical mineral deposits and form under mineralising fluid activities,” Dr Zhou said.

“Our work shows that we can trace the history of fluids in the Earth’s crust and see when and what mineral resources they might generate.”

The renewable energy sector is continuing to grow rapidly with increasing demand for technologies like wind turbines, solar panels, electric vehicles and batteries.

“These often require large quantities of critical minerals,” he said.

“Electric vehicles need up to four times more copper than conventional cars and a single wind turbine uses several tonnes of permanent magnets made of rare earth metals.”

Dr Zhou said being able to study and discover these minerals was going to become increasingly important.

“Researchers across many institutions are doing excellent work in this field, including UQ’s Centre for Geoanalytical Mass Spectrometry,” Dr Zhou said.

“Our hope is to expand our collaboration with industry and academia to increase the understanding and discovery of critical minerals in the future.”

This research has been published in Geochronology and Communications Earth & Environment.

Journal/
conference:
Geochronology, Communications Earth & Environment
Research:Paper
Organisation/s: The University of Queensland
Funder: Geochronology paper: The project was funded by Deutsche Forschungsgemeinschaft e.V. (DFG) grant SO 436/12-1 to Edward R. Sobel and DFG grant KL 495/27-1 to Jonas Kley. Additional support was provided by grants to Edward R. Sobel, Jian-Xin Zhao, and Renjie Zhou through the Australia–Germany Joint Research Cooperation Scheme, to Daryl L. Howard and Renjie Zhou through the Australian Synchrotron Access Program and to Renjie Zhou through a UQ ECR grant. Jie Chen was supported by grants through the Second Tibetan Plateau Scientific Expedition and Research Program (STEP, 2019QZKK0901) and State Key Laboratory of Earthquake Dynamics of China (LED2016A05). Communications Earth & Environment paper: G.A. is supported by a postdoctoral fellowship of the Swiss National Science Foundation (grant no. 178098) and the Robert Day Postdoctoral Fellowship in Palaeontology and Stratigraphy of the University of Queensland. R.Z. is supported by a UQ ECR grant
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