Robert J. Tracy
About
In The Last Decade
Robert J. Tracy
62 papers receiving 1.8k citations
Peers
Comparison fields: 5 of 93
- Geophysics 1.8k
- Artificial Intelligence 527
- Geochemistry and Petrology 220
- Atmospheric Science 180
- Paleontology 127
Countries citing papers authored by Robert J. Tracy
This map shows the geographic impact of Robert J. Tracy'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 Robert J. Tracy with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Robert J. Tracy more than expected).
Fields of papers citing papers by Robert J. Tracy
This network shows the impact of papers produced by Robert J. Tracy. 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 Robert J. Tracy. The network helps show where Robert J. Tracy may publish in the future.
Co-authorship network of co-authors of Robert J. Tracy
This figure shows the co-authorship network connecting the top 25 collaborators of Robert J. Tracy. A scholar is included among the top collaborators of Robert J. Tracy 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 Robert J. Tracy. Robert J. Tracy is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 0 | |
| 2 | 3 | |
| 3 | GARNET GROWTH ZONING IN METAPELITES: NOT SO SIMPLE AFTER ALL, AND REVEALING MORE THAN WE ONCE THOUGHT? | 1 |
| 4 | High Pressure Crystallization of Mafic Magma: Field Observations, Compositional Measurements and Computer Modeling | 1 |
| 5 | Direct Comparison of Monazite Ages Obtained By in situ Techniques: Ion-Probe Isotopic Ages Versus Electron Microprobe Chemical Ages | 1 |
| 6 | 25 | |
| 7 | Ba-rich micas from the Franklin Marble, Lime Crest and Sterling Hill, New Jersey | 45 |
| 8 | Phase equilibria and thermobarometry of metapelites | 150 |
| 9 | Phase equilibria and thermobarometry of calcareous, ultramafic and mafic rocks, and iron formations | 81 |
| 10 | The Influence of Adult Encouragement on Children's Persistence. | 4 |
| 11 | 2 | |
| 12 | High-temperature retrograde reactions in pelitic gneiss, central Massachusetts | 24 |
| 13 | Compositional zoning and inclusions in metamorphic minerals | 268 |
| 14 | A pyrope-spinel (alkremite) xenolith from Moses Rock Dike; first known North American occurrence | 13 |
| 15 | Monticellite marble at Cascade Mountain, Adirondack Mountains, New York | 18 |
| 16 | Orthoferrosilite and other iron-rich pyroxenes in microperthite gneiss of the Mount Marcy area, Adirondack Mountains | 27 |
| 17 | Zoned titanian augite in alkali olivine basalt from Tahiti and the nature of titanium substitutions in augite | 46 |
| 18 | High pressure sillimanite-garnet-biotite assemblage formed by recrystallization of mylonite in sillimanite-cordierite-biotite-orthoclase schist, central Massachusetts | 2 |
| 19 | Garnet composition and zoning in the determination of temperature and pressure of metamorphism, central Massachusetts | 286 |
| 20 | Orientation of Pigeonite Exsolution Lamellae in Metamorphic Augite: Correlation with Composition and Calculated Optimal Phase Boundaries | 27 |
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.