W. Compston
About
In The Last Decade
W. Compston
201 papers receiving 17.0k citations
Hit Papers
Peers
Comparison fields: 5 of 111
- Geophysics 15.6k
- Artificial Intelligence 6.6k
- Paleontology 3.1k
- Atmospheric Science 3.1k
- Geochemistry and Petrology 2.8k
Countries citing papers authored by W. Compston
This map shows the geographic impact of W. Compston'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 W. Compston with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites W. Compston more than expected).
Fields of papers citing papers by W. Compston
This network shows the impact of papers produced by W. Compston. 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 W. Compston. The network helps show where W. Compston may publish in the future.
Co-authorship network of co-authors of W. Compston
This figure shows the co-authorship network connecting the top 25 collaborators of W. Compston. A scholar is included among the top collaborators of W. Compston 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 W. Compston. W. Compston is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 133 | |
| 2 | Discussion on dating the Late Precambrian volcanicity of England and Wales: Reply to J. Horak | 1 |
| 3 | The Problem of Lunar Initial Pb | 1 |
| 4 | Growth of early archaean crust in the ancient Gneiss complex of Swaziland and adjacent Barberton Greenstone Belt, Southern Africa | 6 |
| 5 | 73235,82 (pomegranate): an Assemblage of Lunar Zircon with Unique Overgrowth | 10 |
| 6 | Magnesium Isotopic Systematics of Murchison Refractory Inclusions | 1 |
| 7 | Lunar Zircon and the Closure Age of the Lunar Crust | 6 |
| 8 | Age and Chemistry of Zircon from Late-Stage Lunar Differentiates | 12 |
| 9 | U-Pb Geochronology of Zircons from Breccia 73217 Using a Sensitive High Mass-Resolution Ion Microprobe (shrimp) | 14 |
| 10 | The Interpretation of Scattered Rb-Sr Isotopic Data for Early Archean Gneisses from Labrador and Greenland | 3 |
| 11 | Consortium breccia 73255 - Petrology, major- and trace-element chemistry, and Rb-Sr systematics of aphanitic lithologies | 13 |
| 12 | Rb-Sr systematics ion clasts and aphanites from consortium breccia 73215. | 1 |
| 13 | Titanium Isotope Ratios in Terrestrial and Allende Materials | 4 |
| 14 | REE Trends and Rb-Sr Model Ages in Mare Basalts | 1 |
| 15 | RB-SR Model Ages & Chemical Composition of Nine Apollo 16 Soils | 3 |
| 16 | Age and Petrogenesis of Apollo 14 Basalts | 7 |
| 17 | Apollo 14 mineral ages and the thermal history of the Fra Mauro formation. | 18 |
| 18 | "Chemistry and Rb- Sr ages for Apollo 12 lunar material" | 1 |
| 19 | Rubidium-strontium chronology and chemistry of lunar material from the Ocean of Storms | 60 |
| 20 | The chemistry and age of Apollo 11 lunar material | 55 |
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.