Ray E. Wells
About
In The Last Decade
Ray E. Wells
114 papers receiving 3.4k citations
Peers
Comparison fields: 5 of 63
- Geophysics 3.6k
- Atmospheric Science 1.1k
- Artificial Intelligence 389
- Molecular Biology 306
- Earth-Surface Processes 244
Countries citing papers authored by Ray E. Wells
This map shows the geographic impact of Ray E. Wells'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 Ray E. Wells with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Ray E. Wells more than expected).
Fields of papers citing papers by Ray E. Wells
This network shows the impact of papers produced by Ray E. Wells. 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 Ray E. Wells. The network helps show where Ray E. Wells may publish in the future.
Co-authorship network of co-authors of Ray E. Wells
This figure shows the co-authorship network connecting the top 25 collaborators of Ray E. Wells. A scholar is included among the top collaborators of Ray E. Wells 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 Ray E. Wells. Ray E. Wells 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 | 23 | |
| 3 | Longevity of Yellowstone hotspot volcanism: Isotopic evidence linking the Siletzia LIP (56 Ma) and early Columbia River Basalt Group (17 Ma) mantle sources | 2 |
| 4 | High-Magnitude (>Mw8.0) Megathrust Earthquakes and the Subduction of Thick Sediment, Tectonic Debris, and Smooth Sea Floor | 1 |
| 5 | Seismicity, topography, and free-air gravity of the Aleutian-Alaska subduction zone | 1 |
| 6 | Geologic Mapping and Paired Geochemical-Paleomagnetic Sampling of Reference Sections in the Grande Ronde Basalt: An Example from the Bingen Section, Columbia River Gorge, Washington | 1 |
| 7 | Eastern boundary of the Siletz terrane in the Puget Lowland from gravity and magnetic modeling with implications for seismic hazard analysis | 1 |
| 8 | New Paleomagnetic and Geochemical Reference Sections in Miocene Grande Ronde Basalt Flows on the Columbia Plateau are Fundamental to Stratigraphic, Structural, and Tectonic Studies in the Portland Metro Area and Coast Ranges of Oregon and Washington | 2 |
| 9 | 13 | |
| 10 | 11 | |
| 11 | The Transition Between N-S and NE-SW Directed Crustal Shortening in the Central and Northern Puget Lowland: New Thoughts on the Southern Whidbey Island Fault | 1 |
| 12 | Megathrust Slip and the Care and Feeding of the Subduction Channel Through which the Seismogenic Zone Runs | 4 |
| 13 | The Cottage Lake Lineament, Washington: Onshore Extension of the Southern Whidbey Island Fault? | 0 |
| 14 | Cascadia Gravity and Magnetic Anomalies Delineate Hydrated Forearc Mantle | 1 |
| 15 | Coseismic Slip Beneath Forearc Basins in Great Subduction Zone Earthquakes: Implications for the Size and Mode of Rupture on the Cascadia Subduction Zone | 0 |
| 16 | Life and Death of the Resurrection Plate: Evidence for an Additional Plate in the NE Pacific in Paleocene-Eocene Time | 4 |
| 17 | Effective Transition Zone and Revised 3-D Dislocation Model of Interseismic Deformation for the Cascadia Subduction Zone | 0 |
| 18 | 2 | |
| 19 | Tectonic implications of a high-resolution aeromagnetic survey of the Portland basin, Oregon and Washington | 1 |
| 20 | 53 |
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.