John M. Sinton
About
In The Last Decade
John M. Sinton
112 papers receiving 6.0k citations
Hit Papers
Peers
Comparison fields: 5 of 89
- Geophysics 5.7k
- Atmospheric Science 1.3k
- Artificial Intelligence 798
- Geology 498
- Geochemistry and Petrology 419
Countries citing papers authored by John M. Sinton
This map shows the geographic impact of John M. Sinton'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. Sinton 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. Sinton more than expected).
Fields of papers citing papers by John M. Sinton
This network shows the impact of papers produced by John M. Sinton. 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. Sinton. The network helps show where John M. Sinton may publish in the future.
Co-authorship network of co-authors of John M. Sinton
This figure shows the co-authorship network connecting the top 25 collaborators of John M. Sinton. A scholar is included among the top collaborators of John M. Sinton 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. Sinton. John M. Sinton is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 2 | |
| 2 | 8 | |
| 3 | 11 | |
| 4 | 4 | |
| 5 | Growth History of Kaena Volcano, the Isolated, Dominantly Submarine, Precursor Volcano to Oahu, Hawaii | 0 |
| 6 | 25 | |
| 7 | Resolving Volcanic Eruptions: New Fine-scale Mapping by AUV Sentry of Galápagos Spreading Center 92°W and 95°W | 1 |
| 8 | The ridge filter: How melt supply and magma chambers modulate mantle compositions in MORB | 1 |
| 9 | Investigating the role of magma supply on crustal accretion processes: Seismic structure and axial morphology of the western Galapagos Spreading Center | 2 |
| 10 | Helium Isotope Variations and Mantle Plume-Spreading Ridge Interaction Along the Galapagos Spreading Center | 1 |
| 11 | Geologic Mapping, Volcanic Stages and Magmatic Processes in Hawaiian Volcanoes | 4 |
| 12 | Magma Reservoir Dynamics and Diverse Mantle Melting at the Southern East Pacific Rise: 17° 22'S-17° 35'S | 3 |
| 13 | 1 | |
| 14 | Age Progression and Changes in Mantle Source Composition With Time in the Rano Rahi Seamount Field, East Pacific Rise Flank, 15° -{19° S | 1 |
| 15 | Shallow Crustal Structure Along the Western Galapagos Spreading Center 91.3° to 95.2° W: Correlations Between Axial Magma Lens, Layer 2A and Topographic Characteristics | 4 |
| 16 | Plume-Ridge Interaction along the Galápagos Spreading Center | 2 |
| 17 | Plume-Affected Geochemical Trends in Along-Axis Samples from the Galápagos Spreading Center, 90° 30'W to 98° W | 1 |
| 18 | Correlated Geophysical, Geochemical and Volcanological Manifestations of Plume-Ridge Interaction Along the Galápagos Spreading Center, 90.5-98° W | 2 |
| 19 | Post-Glacial Eruptive History of the Western Volcanic Zone, Iceland | 7 |
| 20 | 7 |
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.