por José Ignacio Canudo | 18/06/2023
Secciones de cristales de estibina, con la exfoliación típica visible. Es poco frecuente en este yacimiento, ya que, aunque fue el sulfuro formado inicialmente, la mayor parte se ha transformado en una mezcla de zinkenita y de esfalerita. Ejemplar, 4,7 cm. Mina Nueva Virginia en Lazuela (Teruel). Foto y colección de Miguel Calvo
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