The Chromite Group is a mineralogical class of oxide minerals crystallizing in the cubic system with the general formula AB₂O₄, distinguished by its specific spinel-type crystal structure and composition wherein A is typically a divalent cation such as Fe²⁺ or Mg²⁺ and B is a trivalent cation predominantly Cr³⁺.
341
Publications
16.4K
Citations
901
Authors
377
Institutions
Publications per year
2017–2026
46
Variants
Chromite Spinel Group
Parents
Publications
341
1–5 of 341
Authors
901
- FZ
15
h-index
- SA
9
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- GG
9
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- GG
8
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- HM
7
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1–5 of 901
Institutions
377
Montanuniversität Leoben
Leoben, Austria
12 h-index
23 publications
1.4K citations
Chinese Academy of Sciences
Beijing, China
11 h-index
33 publications
1.8K citations
University of the Witwatersrand
Johannesburg, South Africa
11 h-index
21 publications
1.8K citations
Russian Academy of Sciences
Moscow, Russia
9 h-index
15 publications
606 citations
Planetary Science Institute
Tucson, United States
9 h-index
19 publications
1.6K citations
Bureau de Recherches Géologiques et Minières
Orléans, France
9 h-index
12 publications
683 citations
Kanazawa University
Kanazawa, Japan
9 h-index
19 publications
1K citations
University of Modena and Reggio Emilia
Modena, Italy
8 h-index
11 publications
723 citations
1–8 of 377
Venues
- Economic Geology
29 publications · 2.1K citations
22
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- American Mineralogist
24 publications · 726 citations
18
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- Mineralium Deposita
20 publications · 1.2K citations
17
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- The Canadian Mineralogist
20 publications · 663 citations
15
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- Ore Geology Reviews
17 publications · 543 citations
15
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1–5