John M. Ferry
About
In The Last Decade
John M. Ferry
102 papers receiving 8.3k citations
Hit Papers
Peers
Comparison fields: 5 of 103
- Geophysics 7.7k
- Artificial Intelligence 2.7k
- Geochemistry and Petrology 1.2k
- Paleontology 1.1k
- Atmospheric Science 1.1k
Countries citing papers authored by John M. Ferry
This map shows the geographic impact of John M. Ferry'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 John M. Ferry with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites John M. Ferry more than expected).
Fields of papers citing papers by John M. Ferry
This network shows the impact of papers produced by John M. Ferry. 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 John M. Ferry. The network helps show where John M. Ferry may publish in the future.
Co-authorship network of co-authors of John M. Ferry
This figure shows the co-authorship network connecting the top 25 collaborators of John M. Ferry. A scholar is included among the top collaborators of John M. Ferry 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 John M. Ferry. John M. Ferry is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 40 | |
| 2 | 2 | |
| 3 | 1 | |
| 4 | Role of fluid flow in the contact metamorphism of siliceous dolomitic limestones | 45 |
| 5 | Models for coupled fluid flow, mineral reaction, and isotopic alteration during contact metamorphism; the Notch Peak aureole, Utah | 56 |
| 6 | Carbon and oxygen isotope geochemistry of chlorite-zone rocks of the Waterville Limestone, Maine, U.S.A. | 21 |
| 7 | Highly aluminous hornblende from low-pressure metacarbonates and a preliminary thermodynamic model for the Al content of calcic amphibole | 19 |
| 8 | Metamorphic hydrology at 13-km depth and 400-550 degrees C | 45 |
| 9 | Phase transitions in calcic plagioclase; a correction and further discussion | 3 |
| 10 | Crystal size distributions in Metamorphic rocks | 1 |
| 11 | Phase composition as a measure of reaction progress and an experimental model for the high-temperature metamorphism of mafic igneous rocks | 7 |
| 12 | A TEM study of the biotite-chlorite reaction and comparison with petrologic observations | 116 |
| 13 | Mineral reactions and element migration during metamorphism of calcareous sediments from the Vassalboro Formation, south-central Maine | 42 |
| 14 | Buffering, infiltration, and the control of intensive variables during metamorphism | 71 |
| 15 | Linear algebraic manipulation of n-dimensional composition space | 33 |
| 16 | Characterization of metamorphic fluid composition through mineral equilibria | 45 |
| 17 | Petrology of graphitic sulfide-rich schists from South-central Maine: an example of desulfidation during prograde regional metamorphism | 113 |
| 18 | A comparative study of geothermometers and geobarometers in pelitic schists from South-central Maine | 69 |
| 19 | A map of chemical potential differences within an outcrop | 31 |
| 20 | Subsolidus phase relations in the nepheline-kalsilite system at 0.5, 2.0, and 5.0 kbar | 22 |
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.