Crisógono Vásconcelos
About
In The Last Decade
Crisógono Vásconcelos
72 papers receiving 5.4k citations
Hit Papers
Peers
Comparison fields: 5 of 99
- Paleontology 3.5k
- Atmospheric Science 2.2k
- Environmental Chemistry 1.5k
- Geochemistry and Petrology 1.4k
- Mechanics of Materials 1.1k
Countries citing papers authored by Crisógono Vásconcelos
This map shows the geographic impact of Crisógono Vásconcelos's research. It shows the number of citations coming from papers published by authors working in each country. You can also color the map by specialization and compare the number of citations received by Crisógono Vásconcelos with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Crisógono Vásconcelos more than expected).
Fields of papers citing papers by Crisógono Vásconcelos
This network shows the impact of papers produced by Crisógono Vásconcelos. Nodes represent research fields, and links connect fields that are likely to share authors. Colored nodes show fields that tend to cite the papers produced by Crisógono Vásconcelos. The network helps show where Crisógono Vásconcelos may publish in the future.
Co-authorship network of co-authors of Crisógono Vásconcelos
This figure shows the co-authorship network connecting the top 25 collaborators of Crisógono Vásconcelos. A scholar is included among the top collaborators of Crisógono Vásconcelos based on the total number of citations received by their joint publications. Widths of edges represent the number of papers authors have co-authored together. Node borders signify the number of papers an author published with Crisógono Vásconcelos. Crisógono Vásconcelos is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 1 | |
| 2 | 1 | |
| 3 | 3 | |
| 4 | 50 | |
| 5 | Subsurface dolomite formation during post-depositional flow of sulphate-bearing fluids from underlying salt giants: Early Pliocene example at DSDP Leg 42A, Site 374, Ionian Abyssal Plain | 0 |
| 6 | Methanogenesis produces strong 13C-enrichment in stromatolites of Lagoa Salgada, Brazil: A modern analogue for Palaeo-/Neoproterozoic stromatolites? | 2 |
| 7 | Clay Mineral Assemblages as Proxies for Reconstructing Messinian Paleoenvironments in the Western Mediterranean | 1 |
| 8 | 77 | |
| 9 | 281 | |
| 10 | Dolomite as a Biomineral and Possible Implications | 6 |
| 11 | 142 | |
| 12 | The Role of Extracellular Polymeric Substances in the Nucleation of Microbial Dolomite | 1 |
| 13 | Evidences of microbial mediation in the formation of MDAC in the Gulf of Cadiz | 2 |
| 14 | Magnesium Isotopic Evidence for Widespread Microbial Dolomite Precipitation in the Geological Record. | 2 |
| 15 | Bacterially Induced Dolomite Formation in the Presence of Sulfate Ions under Aerobic Conditions | 2 |
| 16 | Lithifying microbial mats in Lagoa Vermelha, Brazil: A model system for Precambrian carbonate formation? | 2 |
| 17 | Microbial Mediated Mineralization in the Extreme Hypersaline Sabkha Environment of Abu Dhabi (UAE) | 1 |
| 18 | 62 | |
| 19 | Precipitation of Dolomite in Aerobic Culture Experiments Using Halophilic Bacteria | 1 |
| 20 | Microbial mediation of modern dolomite precipitation and diagenesis under anoxic conditions | 42 |
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive bibliographic database. While OpenAlex provides broad and valuable coverage of the global research landscape, it—like all bibliographic datasets—has inherent limitations. These include incomplete records, variations in author disambiguation, differences in journal indexing, and delays in data updates. As a result, some metrics and network relationships displayed in Rankless may not fully capture the entirety of a scholar's output or impact.