Edward Olsen
About
In The Last Decade
Edward Olsen
59 papers receiving 1.6k citations
Peers
Comparison fields: 5 of 73
- Astronomy and Astrophysics 1.4k
- Geophysics 807
- Ecology 343
- Atmospheric Science 169
- Nuclear and High Energy Physics 155
Countries citing papers authored by Edward Olsen
This map shows the geographic impact of Edward Olsen'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 Edward Olsen with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Edward Olsen more than expected).
Fields of papers citing papers by Edward Olsen
This network shows the impact of papers produced by Edward Olsen. 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 Edward Olsen. The network helps show where Edward Olsen may publish in the future.
Co-authorship network of co-authors of Edward Olsen
This figure shows the co-authorship network connecting the top 25 collaborators of Edward Olsen. A scholar is included among the top collaborators of Edward Olsen 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 Edward Olsen. Edward Olsen is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 49 | |
| 2 | Tambo Quemado: Extraordinary concentrations of REE and refractory trace elements caused by artificial heating | 1 |
| 3 | CR Isotopes in Differentiated Meteorites: Evidence for 53Mn | 7 |
| 4 | Anomalous ataxite from Mount Howe, Antarctica | 6 |
| 5 | 26 | |
| 6 | Globular Silicate Inclusions in IIE Irons and Sombrerete: Highly Fractionated Minimum Melts | 10 |
| 7 | 30 | |
| 8 | A Mg Isotope Study of Hibonite-Bearing Murchison Inclusions | 4 |
| 9 | Refractory Inclusions in Murchison: Recovery and Mineralogical Description | 12 |
| 10 | Refractory Inclusions in Murchison: Chemistry and MG Isotopic Composition | 4 |
| 11 | Murchison: Composition Relations Between Isolated Grains and Aggregates | 2 |
| 12 | Chemical Studies of Condensates in the Murchison Type 2 Carbonaceous Chondrite | 7 |
| 13 | Happy Canyon: An E-7 enstatite chondrite | 1 |
| 14 | New X-Ray and Compositional Data for Farringtonite, Mg3(PO4)2 | 9 |
| 15 | Ortho- and clinopyroxene compositions in ordinary chondrites and related blander model calculation procedures | 6 |
| 16 | Empirical derivation of activity coefficients for the magnesium-rich portion of the olivine solid solution | 9 |
| 17 | Mineralogy and composition of the Murchison meteorite. | 8 |
| 18 | Compositions of natural osumilites | 17 |
| 19 | A new occurrence of roedderite and its bearing on osumilite-type minerals | 12 |
| 20 | 14 |
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.