oxidos e hidroxidos
En general, su estudio se realiza mediante microscopia de luz reflejada ya que la mayor parte de ellos (ilmenita, magnetita, etc..) se comportan como opacos en el microscopio de luz transmitida. Algunos óxidos como el rutilo (TiO2), los minerales del grupo de las espinelas (MgAl2O4) o el corindón (Al2O3) pueden aparecer como accesorios en rocas comunes.
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