Gary Stevens
About
In The Last Decade
Gary Stevens
133 papers receiving 5.9k citations
Hit Papers
Peers
Comparison fields: 5 of 102
- Geophysics 5.7k
- Artificial Intelligence 2.9k
- Geochemistry and Petrology 649
- Paleontology 377
- Geology 338
Countries citing papers authored by Gary Stevens
This map shows the geographic impact of Gary Stevens'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 Gary Stevens with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Gary Stevens more than expected).
Fields of papers citing papers by Gary Stevens
This network shows the impact of papers produced by Gary Stevens. 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 Gary Stevens. The network helps show where Gary Stevens may publish in the future.
Co-authorship network of co-authors of Gary Stevens
This figure shows the co-authorship network connecting the top 25 collaborators of Gary Stevens. A scholar is included among the top collaborators of Gary Stevens 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 Gary Stevens. Gary Stevens is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 2 | |
| 2 | 2 | |
| 3 | 1 | |
| 4 | 8 | |
| 5 | 35 | |
| 6 | Contrasting petrogenesis of Mg-K and Fe-K granitoids and implications for post-collisional magmatism: case study from the late-Archaean Matok pluton (South Africa) | 1 |
| 7 | 26 | |
| 8 | 40 | |
| 9 | A 3.2 Ga Magmatic arc Preserving 50 Ma of Crustal Convergence in the Barberton Terrain, South Africa | 2 |
| 10 | 87 | |
| 11 | 207 | |
| 12 | Chemical Variations in Granitic Magmas: Source-inherited or Products of Magmatic Processes? | 2 |
| 13 | Where are the TTG formed? A review of geochemical and experimental data. | 1 |
| 14 | Timing of mid- to lower-crustal metamorphism in the granitoid-gneiss terrain south of the Barberton greenstone belt, South Africa | 1 |
| 15 | A Whole-Rock Oxygen-Isotopic Analysis of the Core Region of the Vredefort Structure, South Africa | 1 |
| 16 | Pre- and Postimpact Metamorphism in the Core of the Vredefort Dome: Clues to Crustal Response at a Massive Meteorite Strike | 2 |
| 17 | Metamorphism and Alteration of West Rand Group Shales from Distal Portions of the Witwatersrand Basin: Consequences for a Basin-wide Metamorphic Model | 2 |
| 18 | Impact-related Metamorphism in the Vredefort Dome, South Africa | 1 |
| 19 | Metamorphism, fluid-flow, and gold mobilization in the Witwatersrand Basin; towards a unifying model | 15 |
| 20 | Alteration, heat, and Witwatersrand gold; 111 years after Harrison and Langlaagte | 22 |
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.