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Discovery of crystalline Fe2O3 in returned lunar soils
Abstract Lunar materials were believed to have formed and been preserved in a reducing environment, with only Fe2+ and Fe0 present. Native oxidized minerals, such as hematite, have not been validated in previously returned lunar samples. In this work, we report the discovery of micrometer-scale crystalline Fe2O3 in the forms of hematite (α-Fe2O3) and maghemite (γ-Fe2O3) overgrowing troilite in the recently returned Chang’e-6 (CE6) lunar soils.
3D Digital Holography Investigations of Giant Photostriction Effect in MAPbBr3 Perovskite Single Crystals (Adv. Funct. Mater. 44/2024)
Zongcheng Ling Shandong Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, School of Space Science and Physics, Institute of Space Sciences, Shandong University, Weihai, 264209 China Search for more papers by this author
Sensors | Free Full-Text | Pseudo-Spectral Spatial Feature Extraction and Enhanced Fusion Image for Efficient Meter-Sized Lunar Impact Crater Automatic Detection in Digital Orthophoto Map
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