Thomas Pettke
About
In The Last Decade
Thomas Pettke
210 papers receiving 14.4k citations
Hit Papers
Peers
Comparison fields: 5 of 110
- Geophysics 12.3k
- Artificial Intelligence 5.5k
- Geochemistry and Petrology 2.5k
- Atmospheric Science 1.3k
- Mechanics of Materials 1.0k
Countries citing papers authored by Thomas Pettke
This map shows the geographic impact of Thomas Pettke'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 Thomas Pettke with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Thomas Pettke more than expected).
Fields of papers citing papers by Thomas Pettke
This network shows the impact of papers produced by Thomas Pettke. 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 Thomas Pettke. The network helps show where Thomas Pettke may publish in the future.
Co-authorship network of co-authors of Thomas Pettke
This figure shows the co-authorship network connecting the top 25 collaborators of Thomas Pettke. A scholar is included among the top collaborators of Thomas Pettke 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 Thomas Pettke. Thomas Pettke is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 1 | |
| 2 | 9 | |
| 3 | 38 | |
| 4 | Magnetic anisotropy in pyroxene single crystals | 1 |
| 5 | Magnetic Anisotropy of Single Crystals: Amphiboles, Pyroxenes and Feldspars | 1 |
| 6 | Deep subduction fluids and their interaction with the mantle wedge | 1 |
| 7 | Serpentine dehydration recorded by garnet peridotites and chlorite harzburgites from Cima di Gagnone | 1 |
| 8 | The chemical signatures of progressive dehydration stages in subducted serpentinites | 0 |
| 9 | The composition of serpentinite dehydration fluids in subduction zones: An experimental study | 4 |
| 10 | 158 | |
| 11 | Precise and accurate lead isotopic analysis of fast transient signals by laser-ablation MC-ICP-MS | 1 |
| 12 | 2 | |
| 13 | In Situ Laser-Ablation-ICP-MS chemical analysis of melt inclusion and prospects for constraining subduction zone magmatism | 18 |
| 14 | Trace Element Partitioning Between low-Ca Pyroxene and Ultracalcic Liquids. | 1 |
| 15 | Experimental Determination of High-Pressure Fluid Composition in Equilibrium with Residual Eclogite | 1 |
| 16 | The Porphyry to Epithermal Link: Preliminary Fluid Chemical Results from the Apuseni Mountains, Romania, and Famatina, Argentinian Andes | 5 |
| 17 | Characterization of the Magmatic-to-Hydrothermal Transition in Barren vs. Mineralized Granites | 1 |
| 18 | The Chemical Composition and Light-Noble-Gas Data of Halite in the Monahans Regolithic Breccia | 3 |
| 19 | 37 | |
| 20 | Chemical Composition of Halite from the Monahans Chondrite Determined by Laser Ablation ICP-MS | 2 |
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.