The chemical elements were discovered in identified minerals and with the help of the identified elements the mineral crystal structure could be described. Georgius Agricola is considered the 'father of mineralogy'. One milestone was the discovery of the geometrical law of crystallization by René Just Haüy, a further development of the work by Nicolas Steno and Jean-Baptiste L. Romé de l'Isle (the characterisation of a crystalline mineral needs knowledge on crystallography). Other milestones were the notion that metals are elements too (Antoine Lavoisier) and the periodic table of the elements by Dmitri Ivanovich Mendeleev. The overview of the organic bonds by Kekulé was necessary to understand the silicates, first refinements described by Bragg and Machatschki; and it was only possibly to understand a crystal structure with Dalton's atomic theory and Goldschmidt's explanations. Specific gravity, streak (streak color and mineral hardness) and X-ray powder diffraction are quite specific for a Nickel-Strunz identifier (9 ed./10 ed.). Nowadays, non-destructive electron microprobe analysis is used to get the empirical formula of a mineral. Finally, the International Zeolite Association (IZA) took care of the zeolite frameworks (part of molecular sieves and/or molecular cages).
Contents
- Prehistoric Period Before Theophrastus before 400 BC
- Before Agricola c1500
- After Agricola c1500
- After Hays Trait de Minralogy after 1799
- After the World War I gap after 1915
- International Mineralogical Association era after 1957
- IMA Master List of Valid Minerals era after 1999
- Beginnings of the IMA Master List of Minerals
- Mineral names
- The System of Mineralogy of James D Dana
- Glossary of Mineral Species
- Strunz Mineralogical Tables
- Rock Forming Minerals series
- Carl Friedrich Rammelsberg series
- Carl Hintze
- Handbook for chemists and physicists DAns Lax
- Max H Hey
- References
There are only a few thousand mineral species and 83 geochemically stable chemical elements combine to form them. The mineral evolution in the geologic time context were discussed and summarised by A. G. Zhabin (and subsequent Russian workers), Robert M. Hazen, William A. Deer, Robert A. Howie and Jack Zussman.
Prehistoric Period / Before Theophrastus (before 400 BC)
Before Agricola (c. 1500)
After Agricola (c. 1500)
After Haüy's Traité de Minéralogy (after 1799)
After the World War I gap (after 1915)
International Mineralogical Association era (after 1957)
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