D. M. Unruh
About
In The Last Decade
D. M. Unruh
49 papers receiving 1.1k citations
Peers
Comparison fields: 5 of 53
- Geophysics 961
- Astronomy and Astrophysics 316
- Artificial Intelligence 278
- Atmospheric Science 251
- Geochemistry and Petrology 168
Countries citing papers authored by D. M. Unruh
This map shows the geographic impact of D. M. Unruh'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 D. M. Unruh with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites D. M. Unruh more than expected).
Fields of papers citing papers by D. M. Unruh
This network shows the impact of papers produced by D. M. Unruh. 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 D. M. Unruh. The network helps show where D. M. Unruh may publish in the future.
Co-authorship network of co-authors of D. M. Unruh
This figure shows the co-authorship network connecting the top 25 collaborators of D. M. Unruh. A scholar is included among the top collaborators of D. M. Unruh 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 D. M. Unruh. D. M. Unruh is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | Evolution of the Salmon River suture and continental delamination in the Syringa embayment | 4 |
| 2 | Melt Weakening in Crustal-Scale Tectonic Wedging, Southern New England | 1 |
| 3 | REE Abundances and Pb-Pb Isotopic Systematics of the Lunar Meteorite, YAMATO-82192 | 1 |
| 4 | Hafnium and Neodymium Isotopic Constraints on Mare Basalt Genesis | 3 |
| 5 | U-Pb Study of l3 Chondrites: Old Ages or Young Disturbances? | 3 |
| 6 | Excess PB in L-Chondrites is it Terrestrial? | 1 |
| 7 | A Uniform U-Pb Age for L Chondrites and a Method for Correcting for Terrestrial Pb Contamination | 5 |
| 8 | Cm-U and Pu-Xe Chronology of Meteoritic Whitlockite: Confirmation of Live 247CM in Early Solar System | 1 |
| 9 | U-Pb Study of the Richardton H5 Chondrite | 3 |
| 10 | Origin and history of the adcumulate eucrite, Moama as inferred from REE abundances, Sm-Nd and U-Pb systematics | 31 |
| 11 | Evolution History of Lunar Mare Basalts: Apollo 15 Samples Revisited | 4 |
| 12 | Evolution of mare basalts - The complexity of the U-Th-Pb system | 9 |
| 13 | 4.4 b.y.-old clast in Boulder 7, Apollo 17 - A comprehensive chronological study by U-Pb, Rb-Sr and Sm-Nd methods | 57 |
| 14 | Comparative 238U-206Pb, 235U-207Pb, 232Th-208Pb, 206Pb-207Pb and 87Rb-87Sr Ages of Basaltic Achondrites and Early Evolution of the Solar System | 5 |
| 15 | U-Th-Pb systematics of some Apollo 17 lunar samples and implications for a lunar basin excavation chronology. | 34 |
| 16 | U-Th-Pb Systematics of Some Apollo 17 Samples | 4 |
| 17 | The Primitive Nature of the Lunar Crust and the Problem of Initial PB Isotopic Compositions of Lunar Rocks: A Rb-Sr and U-Th-Pb Study of Apollo 16 Samples | 4 |
| 18 | The U-Th-Pb systematics of the Allende carbonaceous chondrite. | 1 |
| 19 | U-Th-Pb systematics of some Apollo 16 lunar samples | 18 |
| 20 | U--Th--Pb and Rb--Sr measurements on some Apollo 14 lunar samples | 23 |
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.