The “chessboard” classification scheme of mineral deposits: Mineralogy and geology from aluminum to zirconium

Laser-induced REE3 + photoluminescence of selected accessory minerals — An “advantageous artefact” in Raman spectroscopy

Sulfidic and non-sulfidic indium mineralization of the epithermal Au–Cu–Zn–Pb–Ag deposit San Roque (Provincia Rio Negro, SE Argentina) — with special reference to the “indium window” in zinc sulfide

In this chapter, we describe internal textures ofcrystals, minerals, and mineral assemblages as detected by Ramanspectroscopy As an introduction, and to underline the motivation ofapplying Raman-based heterogeneity images in the Earth sciences,overviews of the different internal textures and the broad range oftechniques to visualize them are given Second, a number of Ramanexperimental details are discussed; however, only those which are ofparticular relevance to mineralogical applications In particular,the different imaging concepts are compared, and it is argued whyEarth scientists prefer to apply hyperspectral Raman maps whereasdirect images, if applied at all, are rarely used in this fieldAlso, the reader is advised of number of common (and oftenpublished) artfacts related to the Raman analysis of minerals Themain part of this chapter deals with Raman-based imagesapplied in the Earth sciences After a brief general overview, whichagain does not claim to be complete, examples for applications inthree selected areas of research are presented in more detail

Application of Raman-based images in the Earth sciences

The most reactive chemical element, F(2), has been claimed not to occur in nature. First direct evidence from in situ NMR spectroscopy now proves that elemental F(2) indeed occurs in nature as an occlusion in "antozonite" (right in the picture), a variant of fluorite (CaF(2), left).

Occurrence of Difluorine F2 in Nature—In Situ Proof and Quantification by NMR Spectroscopy

Accessory minerals of fluorite and their implication regarding the environment of formation (Nabburg–Wölsendorf fluorite district, SE Germany), with special reference to fetid fluorite (“Stinkspat”)

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Accessory minerals of fluorite and their implication regarding the environment of formation (Nabburg–Wölsendorf fluorite district, SE Germany), with special reference to fetid fluorite (“Stinkspat”)