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Thu, 12 Nov, 2026Updated 03:28 pm IST
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Moon Soil Yields Magnetic Surprise

Scientists discover previously unknown magnetic mineral γ-Fe in Chang'e-6 lunar soil, potentially holding secrets of the Moon's ancient magnetic field

Moon Soil Yields Magnetic Surprise
Photo: Union Carbide, Nuclear Division / wikimedia (CC0)

Scientists studying Chang'e-6 lunar soil have made a groundbreaking discovery, uncovering a previously unknown magnetic mineral called γ-Fe. This form of metallic iron has the ability to preserve a stable magnetic signal, potentially acting as a microscopic fossil of the Moon's long-lost magnetic field.

The study, led by Prof. Haifeng Du of the High Magnetic Field Laboratory at the Hefei Institutes of Physical Science, was published in the Proceedings of the National Academy of Sciences on September 16. The researchers used advanced techniques such as focused ion beam preparation, transmission electron microscopy, and chemical analysis to examine the samples.

The team found evidence that the unusual conditions produced by impacts on the Moon may allow γ-Fe to survive at the lunar surface. They proposed that several factors could help stabilize the structure of γ-Fe, including small amounts of carbon and other elements, the rapid cooling of molten material created during an impact, and protection from the surrounding glassy matrix.

The discovery was made possible by the analysis of metallic iron inside impact glass from Chang'e-6 lunar soil. The researchers identified face-centered cubic γ-Fe for the first time in natural lunar samples, which could provide valuable insights into the Moon's ancient magnetic history.

## Why it matters The Moon no longer generates a global magnetic field, but traces of its ancient magnetism remain locked inside lunar rocks and soil. By studying the magnetic minerals preserved in these materials, scientists can reconstruct how the Moon's magnetic environment changed over time. The discovery of γ-Fe could be a significant step forward in understanding the Moon's magnetic past, and its potential implications for the field of astrogeology are substantial.

The study was conducted by researchers from the High Magnetic Field Laboratory at the Hefei Institutes of Physical Science of the Chinese Academy of Sciences. The findings have the potential to shed new light on the Moon's history and evolution, and could have significant implications for future lunar research and exploration.

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