Limestone Diagenesis
Limestone Diagenesis is a geological process denoting the physical, chemical, and biological modifications undergone by limestone sediments during and after lithification, distinguishing it from diagenetic processes affecting other sedimentary rock types through carbonate-specific reactions such as recrystallization, cementation, and dissolution.
249
Publications
12.3K
Citations
602
Authors
311
Institutions
Publications per year
2017–2026
38
Parents
249
Stable isotopes and limestone lithification
J. D. Hudson · Journal of the Geological Society · 1977 · 691 citations
1–5 of 249
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Friedrich-Alexander-Universität Erlangen-Nürnberg, Germany
4 publications · 158 citations
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5
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311

Centre National de la Recherche Scientifique
Paris, France
8 h-index
28 publications
1.6K citations
The University of Texas at Austin
Austin, United States
6 h-index
9 publications
630 citations
University of Cambridge
Cambridge, United Kingdom
6 h-index
6 publications
202 citations
Friedrich-Alexander-Universität Erlangen-Nürnberg
Erlangen, Germany
5 h-index
9 publications
198 citations

University of Liverpool
Liverpool, United Kingdom
5 h-index
5 publications
995 citations

University of Waikato
Hamilton, New Zealand
4 h-index
8 publications
189 citations

Polish Academy of Sciences
Warsaw, Poland
4 h-index
6 publications
208 citations
University of Miami
Coral Gables, United States
4 h-index
7 publications
706 citations
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JSR · 49 publications · 2.5K citations
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25 publications · 1.2K citations
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16 publications · 914 citations
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14 publications · 429 citations
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7 publications · 322 citations
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