Spectroscopy and chemical bonding in the opaque minerals

Research output: Chapter in Book/Conference proceedingChapterpeer-review

Abstract

The rock-forming minerals which are abundant at the Earth's surface are chiefly translucent silicates and carbonates. Opaque minerals occur as minor components in many rocks and the ore minerals, raw materials for the world supplies of metals, are mostly opaque phases. The major categories of opaque minerals are: (i) native metals, semimetals and alloys; (ii) metal sulphides and other chalcogenides (compounds of metals with Se, Te, As, Sb, Bi); (iii) oxides of certain elements, notably the transition metals: (iv) certain hydroxides and oxysalts.
Original languageEnglish
Title of host publicationChemical Bonding and Spectroscopy in Mineral Chemistry
EditorsFrank J. Berry, David J. Vaughan
Place of PublicationDordrecht
PublisherSpringer Nature Netherlands
Pages251-292
Number of pages42
ISBN (Electronic)9789400948389
ISBN (Print)9789401086455
DOIs
Publication statusPublished - 1 Jan 1985

Keywords

  • Specular reflectance
  • Mineral chemistry
  • Energy level diagram
  • Opaque mineral
  • Molecular orbital calculation

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