Paul T. Robinson
About
In The Last Decade
Paul T. Robinson
189 papers receiving 9.8k citations
Hit Papers
Peers
Comparison fields: 5 of 91
- Geophysics 9.8k
- Artificial Intelligence 2.8k
- Geochemistry and Petrology 1.3k
- Paleontology 641
- Atmospheric Science 557
Countries citing papers authored by Paul T. Robinson
This map shows the geographic impact of Paul T. Robinson'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 Paul T. Robinson with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Paul T. Robinson more than expected).
Fields of papers citing papers by Paul T. Robinson
This network shows the impact of papers produced by Paul T. Robinson. 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 Paul T. Robinson. The network helps show where Paul T. Robinson may publish in the future.
Co-authorship network of co-authors of Paul T. Robinson
This figure shows the co-authorship network connecting the top 25 collaborators of Paul T. Robinson. A scholar is included among the top collaborators of Paul T. Robinson 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 Paul T. Robinson. Paul T. Robinson is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 4 | |
| 2 | 1 | |
| 3 | 5 | |
| 4 | 1 | |
| 5 | 26 | |
| 6 | 22 | |
| 7 | 21 | |
| 8 | 49 | |
| 9 | 5 | |
| 10 | 34 | |
| 11 | Detachment Fault Initiation and Control by Partially Molten Zones in the Lower Ocean Crust | 1 |
| 12 | THE ORIGIN AND SIGNIFICANCE OF CRUSTAL MINERALS IN UPPER MANTLE PERIDOTITES | 2 |
| 13 | Deep origin of the Luobusa ophiolitic peridotites and chromitites in Tibet | 2 |
| 14 | Diamond and moissanite in ophiolitic mantle rocks and podiform chromitites: A deep carbon source? | 2 |
| 15 | Ultrahigh pressure eclogites of the North Qaidam and Altun Mountains, NW China and their protoliths | 20 |
| 16 | Oceanic Lithosphere 4. The origin and evolution of oceanic lithosphere: Magmatic processes at oceanic spreading centres | 2 |
| 17 | OCEANIC LITHOSPHERE 2. The Origin and Evolution of Oceanic Lithosphere: Bathymetry and Morphology of the Ocean Basins | 1 |
| 18 | New Series: The Origin and Evolution of Oceanic Lithosphère | 1 |
| 19 | Low-temperature alteration of the extrusive sequence, Troodos Ophiolite, Cyprus | 29 |
| 20 | A new late Hemingfordian mammal fauna from the John Day Formation, Oregon, and its stratigraphic implications | 10 |
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.