Limonite Deposits is a type of residual ore deposit composed predominantly of hydrous iron oxides formed through the chemical weathering of pre-existing iron-bearing minerals, distinguished by its secondary enrichment and occurrence in supergene environments.
45
Publications
1.5K
Citations
137
Authors
55
Institutions
Publications per year
2017–2026
18
Variants
Limonite Ore Deposits
Parents
Publications
45
1–5 of 45
Authors
137
- KSKenzo Sanematsu
National Institute of Advanced Industrial Science and Technology, Japan
3 publications · 58 citations
3
h-index
- PG
3
h-index
- YH
3
h-index
- XZ
2
h-index
- YS
2
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1–5 of 137
Institutions
55
Central South University
Changsha, China
6 h-index
33 publications
1.4K citations
University of Science and Technology Beijing
Beijing, China
3 h-index
13 publications
337 citations
Northeastern University
Shenyang, China
3 h-index
14 publications
776 citations
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation
Chengdu, China
3 h-index
14 publications
776 citations
Akita University
Akita, Japan
2 h-index
5 publications
106 citations
Hokkaido University
Sapporo, Japan
2 h-index
8 publications
458 citations
Hasanuddin University
Makassar, Indonesia
2 h-index
3 publications
52 citations
United States Geological Survey
Reston, United States
2 h-index
2 publications
58 citations
1–8 of 55
Venues
- Journal of Cleaner Production
5 publications · 305 citations
5
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- Hydrometallurgy
4 publications · 195 citations
4
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- Economic Geology
4 publications · 61 citations
4
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- Mineralogical Magazine and Journal of the Mineralogical Society
2 publications · 115 citations
2
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- Minerals
2 publications · 29 citations
2
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1–5