Kurt N. Constenius
About
In The Last Decade
Kurt N. Constenius
41 papers receiving 830 citations
Peers
Comparison fields: 5 of 41
- Geophysics 628
- Atmospheric Science 253
- Artificial Intelligence 188
- Earth-Surface Processes 183
- Paleontology 106
Countries citing papers authored by Kurt N. Constenius
This map shows the geographic impact of Kurt N. Constenius'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 Kurt N. Constenius with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Kurt N. Constenius more than expected).
Fields of papers citing papers by Kurt N. Constenius
This network shows the impact of papers produced by Kurt N. Constenius. 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 Kurt N. Constenius. The network helps show where Kurt N. Constenius may publish in the future.
Co-authorship network of co-authors of Kurt N. Constenius
This figure shows the co-authorship network connecting the top 25 collaborators of Kurt N. Constenius. A scholar is included among the top collaborators of Kurt N. Constenius 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 Kurt N. Constenius. Kurt N. Constenius 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 | 2 | |
| 3 | 25 | |
| 4 | 18 | |
| 5 | Interplay Between Deformation and Proximal Foreland Sedimentation in the Late Cretaceous Sevier Orogenic Belt | 1 |
| 6 | 33 | |
| 7 | Evidence of a lacustrine origin for laminated marl of the Pliocene Bouse Formation, Milpitas Wash, Blythe Basin, lower Colorado River valley | 1 |
| 8 | 6 | |
| 9 | 3 | |
| 10 | Prolonged high relief in the northern Cordilleran orogenic front during middle and late Eocene extension based on stable isotope paleoaltimetry | 1 |
| 11 | 15 | |
| 12 | Preliminary Depositional and Provenance Records of Mesozoic Basin Evolution and Cenozoic Shortening in the High Andes, La Ramada Fold-Thrust Belt, Southern-Central Andes (32-33°S) | 1 |
| 13 | 27 | |
| 14 | Subsurface Evidence for Late Mesozoic Extension in Western Mongolia: Tectonic and Petroleum Systems Implications | 2 |
| 15 | 60 | |
| 16 | 8 | |
| 17 | Extensional Collapse of the Charleston-Nebo Salient and Its Relationship to Space-Time Variations in Cordilleran Orogenic Belt Tectonism and Continental Stratigraphy | 23 |
| 18 | 20 | |
| 19 | Extensional tectonics of the Cordilleran foreland fold and thrust belt and the Jurassic-Cretaceous Great Valley forearc basin | 11 |
| 20 | Structural Configuration of the Kishenehn Basin Delineated by Geophysical Methods, Northwestern Montana and Southeastern British Columbia | 18 |
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.