Simon M. Peacock
About
In The Last Decade
Simon M. Peacock
72 papers receiving 9.9k citations
Hit Papers
Peers
Comparison fields: 5 of 100
- Geophysics 9.4k
- Artificial Intelligence 1.1k
- Geochemistry and Petrology 513
- Atmospheric Science 395
- Mechanics of Materials 312
Countries citing papers authored by Simon M. Peacock
This map shows the geographic impact of Simon M. Peacock'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 Simon M. Peacock with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Simon M. Peacock more than expected).
Fields of papers citing papers by Simon M. Peacock
This network shows the impact of papers produced by Simon M. Peacock. 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 Simon M. Peacock. The network helps show where Simon M. Peacock may publish in the future.
Co-authorship network of co-authors of Simon M. Peacock
This figure shows the co-authorship network connecting the top 25 collaborators of Simon M. Peacock. A scholar is included among the top collaborators of Simon M. Peacock 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 Simon M. Peacock. Simon M. Peacock is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 4 | |
| 2 | 0 | |
| 3 | 2 | |
| 4 | 15 | |
| 5 | 34 | |
| 6 | 21 | |
| 7 | 1 | |
| 8 | 15 | |
| 9 | 27 | |
| 10 | 11 | |
| 11 | Does the stability of talc in the mantle wedge control the maximum depth of slab-wedge decoupling in subduction zones? | 1 |
| 12 | 21 | |
| 13 | Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing breakdown → | 475 |
| 14 | 163 | |
| 15 | Slab melting during the transition from steep to flat subduction: evidence from numerical models of forearc thermal structure | 2 |
| 16 | An inverted continental Moho and serpentinization of the forearc mantle breakdown → | 530 |
| 17 | Intermediate-Depth Earthquakes in Subducting Slabs are Linked to Metamorphic Dehydration Reactions | 2 |
| 18 | On the Importance of Serpentine in the Subduction Factory | 1 |
| 19 | 116 | |
| 20 | Computer programs for petrologic P-T-t path calculations | 83 |
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.