G. W. Pearce
About
In The Last Decade
G. W. Pearce
69 papers receiving 1.1k citations
Peers
Comparison fields: 5 of 132
- Molecular Biology 571
- Astronomy and Astrophysics 441
- Atmospheric Science 271
- Geophysics 196
- Health, Toxicology and Mutagenesis 91
Countries citing papers authored by G. W. Pearce
This map shows the geographic impact of G. W. Pearce'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 G. W. Pearce with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites G. W. Pearce more than expected).
Fields of papers citing papers by G. W. Pearce
This network shows the impact of papers produced by G. W. Pearce. 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 G. W. Pearce. The network helps show where G. W. Pearce may publish in the future.
Co-authorship network of co-authors of G. W. Pearce
This figure shows the co-authorship network connecting the top 25 collaborators of G. W. Pearce. A scholar is included among the top collaborators of G. W. Pearce 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 G. W. Pearce. G. W. Pearce is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | Apollo 15 deep drill core: trace element and metallic iron abundances in size fractions of sample 15002,170. | 2 |
| 2 | A new magnetic paleointensity value for a "young lunar glass". | 13 |
| 3 | Heating experiments and paleointensity determinations. | 9 |
| 4 | On the origin of sample 70019 and its suitability for lunar magnetic field intensity studies. | 4 |
| 5 | Anomalous acquisition of thermoremanence at 130 C in iron and paleointensity of the Allende meteorite. | 6 |
| 6 | Origin of Magnetization in Lunar Breccias: an Example of Thermal Overprinting | 1 |
| 7 | Some complexities in the determination of lunar paleointensities | 23 |
| 8 | Relationship between nickel and metallic iron contents of Apollo 16 and 17 soils. | 4 |
| 9 | Carbon, Sulfur, Hydrogen, and Metallic Iron Abundances in Apollo 15 and Apollo 17 Basalts | 2 |
| 10 | Effects of water on electrical properties of lunar fines. | 9 |
| 11 | Magnetism of the Apollo 17 Samples | 2 |
| 12 | Magnetic properties and granulometry of metallic iron in lunar breccia 14313 | 12 |
| 13 | Magnetic studies on Apollo 15 and 16 lunar samples | 31 |
| 14 | Magnetism and the Early History of the Moon | 5 |
| 15 | Remanent Magnetization of Lunar Samples | 1 |
| 16 | Cause of Secondary Magnetization in Lunar Samples | 4 |
| 17 | Remanent magnetization of the lunar surface. | 18 |
| 18 | Magnetic properties of Apollo 14 breccias and their correlation with metamorphism. | 23 |
| 19 | Magnetism of two Apollo 12 igneous rocks | 12 |
| 20 | Magnetic studies of lunar samples-breccia and fines | 19 |
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.