最終更新日：2025/11/26
Geologists identified nuffieldite in the slag, noting its orthorhombic-dipyramidal habit and pale creamy white color caused by bismuth, copper, lead, and sulfur.
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Geologists identified nuffieldite in the slag, noting its orthorhombic-dipyramidal habit and pale creamy white color caused by bismuth, copper, lead, and sulfur.
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