Mineral Authigenesis
Mineral Authigenesis is the in situ formation of new minerals within a sedimentary deposit during diagenesis, distinguished from detrital mineral components by precipitating directly from pore fluids under physicochemical conditions characteristic of sediment burial and compaction.
1.9K
Publications
85.4K
Citations
5.2K
Authors
1.3K
Institutions
Publications per year
2017–2026
305
1.9K
Constraints on the Formation of Sedimentary Dolomite
Paul A. Baker, Miriam Kastner · Science · 1981 · 610 citations
Helen Thomas, Ross R. Large, Stuart W. Bull et al. · Economic Geology · 2011 · 420 citations · Full text
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Scottish Universities Environmental Research Centre, United Kingdom
14 publications · 392 citations
12
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11
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Federal Institute for Geosciences and Natural Resources, Germany
11 publications · 354 citations
11
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10
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1.3K

Chinese Academy of Sciences
Beijing, China
29 h-index
202 publications
9.2K citations

Centre National de la Recherche Scientifique
Paris, France
27 h-index
157 publications
5.4K citations
United States Geological Survey
Reston, United States
27 h-index
67 publications
3.6K citations

The University of Western Australia
Perth, Australia
27 h-index
91 publications
3.5K citations
China University of Geosciences
Wuhan, China
25 h-index
116 publications
5.4K citations

Commonwealth Scientific and Industrial Research Organisation
Canberra, Australia
23 h-index
61 publications
2.4K citations

China University of Geosciences (Beijing)
Beijing, China
23 h-index
123 publications
5.3K citations

University of Tasmania
Hobart, Australia
22 h-index
86 publications
9K citations
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83 publications · 6.7K citations
50
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141 publications · 6.9K citations
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JSR · 106 publications · 4K citations
38
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86 publications · 3.4K citations
35
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99 publications · 3.9K citations
34
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