David W. Scholl
About
In The Last Decade
David W. Scholl
133 papers receiving 5.9k citations
Hit Papers
Peers
Comparison fields: 5 of 85
- Geophysics 5.2k
- Atmospheric Science 1.5k
- Geology 1.0k
- Artificial Intelligence 762
- Earth-Surface Processes 723
Countries citing papers authored by David W. Scholl
This map shows the geographic impact of David W. Scholl'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 David W. Scholl with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites David W. Scholl more than expected).
Fields of papers citing papers by David W. Scholl
This network shows the impact of papers produced by David W. Scholl. 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 David W. Scholl. The network helps show where David W. Scholl may publish in the future.
Co-authorship network of co-authors of David W. Scholl
This figure shows the co-authorship network connecting the top 25 collaborators of David W. Scholl. A scholar is included among the top collaborators of David W. Scholl 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 David W. Scholl. David W. Scholl 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 | The Argument that the Oceanic Crust of the Backarc Aleutian Basin (Bering Sea) Is a Terrane of Pacific Oceanic Crust, Possibly the Kula Plate, Accreted to the North American Plate at 50-55 Ma | 1 |
| 3 | High-Magnitude (>Mw8.0) Megathrust Earthquakes and the Subduction of Thick Sediment, Tectonic Debris, and Smooth Sea Floor | 1 |
| 4 | New Magnetic Anomaly Compilation Illuminates the Formation of the Aleutian Basin | 3 |
| 5 | New geophysical constraints on the tectonic history of the Bering Sea | 2 |
| 6 | Did the Bering Sea Form as a Cenozoic Backarc Basin | 2 |
| 7 | Constraints on gas and gas hydrate distribution in the Bering Sea from seismic reflection data | 0 |
| 8 | Seismicity, topography, and free-air gravity of the Aleutian-Alaska subduction zone | 1 |
| 9 | Exploring a Link Between Great and Giant Megathrust Earthquakes and Relative Thickness of Sediment and Eroded Debris in the Subduction Channel to Roughness of Subducted Relief | 7 |
| 10 | Long-Offset Seismic Investigations of the Deep Bering Sea | 1 |
| 11 | Back-arc Seamount Distribution Along the Western Aleutian Volcanic Arc | 1 |
| 12 | Ages of Igneous Basement From the Komandorsky Islands, Far Western Aleutian Ridge | 6 |
| 13 | Estimating the global volume of deeply recycled continental crust at continental collision zones | 1 |
| 14 | Geophysical and Geological Data Document That Sediment Subduction and Subduction Erosion Recycle Large Quantities (Globally 2-3 km3/yr) of Continental Crust to the Mantle Wedge | 1 |
| 15 | Crustal Recylcing at Ocean Margin and Continental Subduction Zones and the Net Accumulation of Continental Crust | 3 |
| 16 | Megathrust Slip and the Care and Feeding of the Subduction Channel Through which the Seismogenic Zone Runs | 4 |
| 17 | Forming a deep-water forearc basin by subduction erosion--exploring this idea for the prominent Aleutian forearc basin | 1 |
| 18 | Coseismic Slip Beneath Forearc Basins in Great Subduction Zone Earthquakes: Implications for the Size and Mode of Rupture on the Cascadia Subduction Zone | 0 |
| 19 | Motion of Hawaiian Hotspot During Formation of the Emperor Seamounts: Initial Results of ODP Leg 197 | 4 |
| 20 | 230 |
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.