Christopher Beaumont
About
In The Last Decade
Christopher Beaumont
159 papers receiving 13.8k citations
Hit Papers
Peers
Comparison fields: 5 of 96
- Geophysics 12.5k
- Earth-Surface Processes 2.7k
- Atmospheric Science 2.0k
- Geology 1.9k
- Mechanics of Materials 1.3k
Countries citing papers authored by Christopher Beaumont
This map shows the geographic impact of Christopher Beaumont'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 Christopher Beaumont with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Christopher Beaumont more than expected).
Fields of papers citing papers by Christopher Beaumont
This network shows the impact of papers produced by Christopher Beaumont. 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 Christopher Beaumont. The network helps show where Christopher Beaumont may publish in the future.
Co-authorship network of co-authors of Christopher Beaumont
This figure shows the co-authorship network connecting the top 25 collaborators of Christopher Beaumont. A scholar is included among the top collaborators of Christopher Beaumont 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 Christopher Beaumont. Christopher Beaumont is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | Influence of rheological layering on the formation of offset basins at inherited weak zones during continental rifting: effects of stiff and pliable layers | 2 |
| 2 | 17 | |
| 3 | Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins breakdown → | 455 |
| 4 | Development of Salt Minibasins under Uneven Sedimentation | 1 |
| 5 | Erosion-Induced Reactivation of the Main Central Thrust zone: Model and Implications for Channel Flow in the Himalayan-Tibetan System | 2 |
| 6 | Styles of continental subduction and collision and their effect on formation and exhumation of UHP rocks | 1 |
| 7 | 87 | |
| 8 | 111 | |
| 9 | Controls on the Asymmetry of Lithosphere Extension: the Role of Frictional-Plastic Strain Softening | 1 |
| 10 | Models for Mid and Lower Crustal Channel Flows | 2 |
| 11 | Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation breakdown → | 1338 |
| 12 | How Will LITHOPROBE's Final Chapter Be Written? | 2 |
| 13 | 25 | |
| 14 | 180 | |
| 15 | Preliminary evidence from apatite fission-track data concerning the thermal history of the Peace River Arch region, Western Canada Sedimentary Basin | 21 |
| 16 | 3 | |
| 17 | 16 | |
| 18 | 57 | |
| 19 | Preliminary Results From a Thermo-Mechanical Model for the Evolution of Atlantic Type Continental Margins | 15 |
| 20 | Tilts and Tides: a Study of the Deformation of the Earth by Ocean Tide Loading. | 3 |
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.