Paul F. Hoffman
About
In The Last Decade
Paul F. Hoffman
119 papers receiving 11.7k citations
Hit Papers
Peers
Comparison fields: 5 of 123
- Geophysics 7.6k
- Paleontology 7.1k
- Atmospheric Science 4.7k
- Geochemistry and Petrology 2.4k
- Artificial Intelligence 1.9k
Countries citing papers authored by Paul F. Hoffman
This map shows the geographic impact of Paul F. Hoffman'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 Paul F. Hoffman with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Paul F. Hoffman more than expected).
Fields of papers citing papers by Paul F. Hoffman
This network shows the impact of papers produced by Paul F. Hoffman. 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 Paul F. Hoffman. The network helps show where Paul F. Hoffman may publish in the future.
Co-authorship network of co-authors of Paul F. Hoffman
This figure shows the co-authorship network connecting the top 25 collaborators of Paul F. Hoffman. A scholar is included among the top collaborators of Paul F. Hoffman 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 Paul F. Hoffman. Paul F. Hoffman 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 | 1 | |
| 3 | 2 | |
| 4 | 2 | |
| 5 | 24 | |
| 6 | An early diagenetic deglacial origin for basal Ediacaran "cap dolostones" | 1 |
| 7 | A CRYOGENIAN-EARLY EDIACARAN CARBONATE SHELF BREAK DOMINATED BY GLACIAL PALEOTOPOGRAPHY, FRANSFONTEIN RIDGE, KUNENE REGION, NAMIBIA | 2 |
| 8 | The Tooth of Time: Alfred Wegener | 1 |
| 9 | The Tooth of Time: How do passive margins become active? | 8 |
| 10 | 166 | |
| 11 | Three for the neoproterozoic: sturtian, marinoan and varangerian glaciations | 3 |
| 12 | Stratigraphic Transition into and out of a Snowball Glacial: Evidence from the Otavi Platform and Fransfontein Slope, Namibia | 3 |
| 13 | Strontium Isotopes in Neoproterozoic Cap Carbonates from Namibia: Evidence for Intense Chemical Weathering in the Aftermath of a Snowball Earth | 1 |
| 14 | 11 | |
| 15 | 12 | |
| 16 | 47 | |
| 17 | Dynamics of the tectonic assembly of northeast Laurentia in geon 18 (1.9-1.8 Ga) | 53 |
| 18 | 104 | |
| 19 | Abner/Denault Reef Complex (2.1 Ga), Labrador Trough, N.E. Quebec | 3 |
| 20 | 122 |
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.