Thomas M. Hearn
About
In The Last Decade
Thomas M. Hearn
52 papers receiving 2.5k citations
Peers
Comparison fields: 5 of 46
- Geophysics 2.7k
- Artificial Intelligence 147
- Geology 80
- Ocean Engineering 65
- Atmospheric Science 49
Countries citing papers authored by Thomas M. Hearn
This map shows the geographic impact of Thomas M. Hearn'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 Thomas M. Hearn with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Thomas M. Hearn more than expected).
Fields of papers citing papers by Thomas M. Hearn
This network shows the impact of papers produced by Thomas M. Hearn. 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 Thomas M. Hearn. The network helps show where Thomas M. Hearn may publish in the future.
Co-authorship network of co-authors of Thomas M. Hearn
This figure shows the co-authorship network connecting the top 25 collaborators of Thomas M. Hearn. A scholar is included among the top collaborators of Thomas M. Hearn 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 Thomas M. Hearn. Thomas M. Hearn is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 3 | |
| 2 | 1 | |
| 3 | Late Cenozoic deformation of the Eurasian and Burma Plates due to subduction of the Indian Plate beneath SE Tibetan Plateau and Myanmar | 2 |
| 4 | 15 | |
| 5 | Three-dimensional variations in the Tibetan mantle lid velocity from Pn tomography | 2 |
| 6 | Pn tomography of eastern Tibet | 1 |
| 7 | Significant Seismic Anisotropy Beneath Northeastern Tibet: Implications for Continuous Deformation processes of eastern Tibet | 1 |
| 8 | Seismic Anisotropy of Northern Tibet: Combine data from Indepth IV array and permanent stations | 0 |
| 9 | Indepth IV Passive Seismic Array: Locating Regional Earthquakes in Northern Tibet | 0 |
| 10 | Upper mantle structure of the Eastern Tibetan Plateau from finite frequency body wave tomography | 0 |
| 11 | Lithospheric Seismic Velocity Structure of the Northern Tibetan Plateau: The ASCENT Seismic Experiment | 4 |
| 12 | Amplitude Tomography From ML-Magnitude Data Beneath China | 1 |
| 13 | Short-period surface-wave amplitude tomography of China | 1 |
| 14 | 25 | |
| 15 | 116 | |
| 16 | 15 | |
| 17 | Crust and Mantle Structure Beneath the INDEPTH-III Central Tibet Array | 1 |
| 18 | 13 | |
| 19 | 167 | |
| 20 | 187 |
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.