T. Ferroir
About
In The Last Decade
T. Ferroir
12 papers receiving 316 citations
Peers
Comparison fields: 5 of 47
- Geophysics 200
- Astronomy and Astrophysics 142
- Materials Chemistry 41
- Ecology 31
- Computational Mechanics 29
Countries citing papers authored by T. Ferroir
This map shows the geographic impact of T. Ferroir'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 T. Ferroir with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites T. Ferroir more than expected).
Fields of papers citing papers by T. Ferroir
This network shows the impact of papers produced by T. Ferroir. 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 T. Ferroir. The network helps show where T. Ferroir may publish in the future.
Co-authorship network of co-authors of T. Ferroir
This figure shows the co-authorship network connecting the top 25 collaborators of T. Ferroir. A scholar is included among the top collaborators of T. Ferroir 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 T. Ferroir. T. Ferroir is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 20 | |
| 2 | 50 | |
| 3 | Evidence for Fractional Crystallization of Wadsleyite and Ringwoodite from Individual Olivine Melt Pockets in Chondrules Entrained in Shock Melt Veins | 0 |
| 4 | 54 | |
| 5 | 31 | |
| 6 | 19 | |
| 7 | Two Contrasting Nucleation and Growth Settings Induced by Dynamic High-Pressure Phase Transitions of Olivine to Ringwoodite and Wadsleyite in Shocked L6-Chondrites | 2 |
| 8 | 37 | |
| 9 | Shock-Melting of Martian Basalts and the Entrapment of Atmospheric Gases | 2 |
| 10 | Intracrystalline and grain-boundary olivine-ringwoodite (-wadsleyite) phase transitions in shocked L6 chondrites: Evidence for diffusion controlled phase transition mechanisms involving Fe and Mn | 1 |
| 11 | 33 | |
| 12 | 37 | |
| 13 | 34 |
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.