Bernard Bingen
About
In The Last Decade
Bernard Bingen
92 papers receiving 5.7k citations
Hit Papers
Peers
Comparison fields: 5 of 71
- Geophysics 5.4k
- Artificial Intelligence 2.3k
- Paleontology 875
- Geochemistry and Petrology 769
- Atmospheric Science 539
Countries citing papers authored by Bernard Bingen
This map shows the geographic impact of Bernard Bingen'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 Bernard Bingen with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Bernard Bingen more than expected).
Fields of papers citing papers by Bernard Bingen
This network shows the impact of papers produced by Bernard Bingen. 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 Bernard Bingen. The network helps show where Bernard Bingen may publish in the future.
Co-authorship network of co-authors of Bernard Bingen
This figure shows the co-authorship network connecting the top 25 collaborators of Bernard Bingen. A scholar is included among the top collaborators of Bernard Bingen 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 Bernard Bingen. Bernard Bingen is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 1 | |
| 2 | A glimpse into upper crustal conditions of an ancient orogen preserved within another; A late-Sveconorwegian volcano-sedimentary sequence in the southwestern Scandinavian Caledonides | 1 |
| 3 | Tectonic basement slices in the décollement of the Scandinavian Caledonides: transition from thin-skinned to thick-skinned tectonics in collisional orogens | 1 |
| 4 | 28 | |
| 5 | 26 | |
| 6 | 33 | |
| 7 | 62 | |
| 8 | 12 | |
| 9 | The Kongsberg-Modum terrane of Southern Norway: a key toward a refined conceptual model of the Sveconorwegian orogen | 2 |
| 10 | Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution breakdown → | 576 |
| 11 | Massif-type anorthosites and related granitoids result from post-collisional remelting of a continental arc root: the Sveconorwegian case | 1 |
| 12 | 34 | |
| 13 | 372 | |
| 14 | 11 | |
| 15 | 165 | |
| 16 | 55 | |
| 17 | Re-Os dating of molybdenite constrains late-orogenic gneiss dome formation in the Sveconorwegian orogen, SW Scandinavia | 2 |
| 18 | 160 | |
| 19 | Monazite and titanite U-Pb dating of Caledonian high-grade metamorphism in the Mid-Scandinavian Caledonides, Norway: a combined SHRIMP and ID-TIMS approach | 1 |
| 20 | 4 |
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.