Max W. Schmidt
About
In The Last Decade
Max W. Schmidt
163 papers receiving 12.5k citations
Hit Papers
Peers
Comparison fields: 5 of 101
- Geophysics 12.0k
- Artificial Intelligence 2.7k
- Geochemistry and Petrology 1.0k
- Materials Chemistry 612
- Astronomy and Astrophysics 605
Countries citing papers authored by Max W. Schmidt
This map shows the geographic impact of Max W. Schmidt'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 Max W. Schmidt with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Max W. Schmidt more than expected).
Fields of papers citing papers by Max W. Schmidt
This network shows the impact of papers produced by Max W. Schmidt. 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 Max W. Schmidt. The network helps show where Max W. Schmidt may publish in the future.
Co-authorship network of co-authors of Max W. Schmidt
This figure shows the co-authorship network connecting the top 25 collaborators of Max W. Schmidt. A scholar is included among the top collaborators of Max W. Schmidt 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 Max W. Schmidt. Max W. Schmidt is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 0 | |
| 2 | 0 | |
| 3 | 3 | |
| 4 | 1 | |
| 5 | 10 | |
| 6 | 37 | |
| 7 | Dihedral angle of carbonatite melts in mantle residue near the upper mantle and transition zone | 1 |
| 8 | Experimental determination of the Mo isotope fractionation factor between metal and silicate liquids | 1 |
| 9 | Constraints on Fe isotope fractionation between liquid metal and liquid silicate from experiments at 1 GPa and 1250-1300°C | 1 |
| 10 | Pt in Silicate Melts: Centrifuging Nanonuggets to Decipher Core Formation Processes | 3 |
| 11 | The Stability of Phase D at High Pressure and Temperature | 1 |
| 12 | Partitioning of protactinium, uranium, thorium and other trace elements between columbite and hydrous silicate melt | 1 |
| 13 | Composition of low-degree hydrous melts of fertile spinel- or garnetbearing lherzolite | 4 |
| 14 | CO2 and potassium in the mantle: carbonaceous pelite melts from the trailing edge of a detached slab hybridizing in the mantle to ultrapotassic kamafugite | 3 |
| 15 | Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth breakdown → | 1181 |
| 16 | Fluid and melt compositions coexisting with eclogite at high pressure and temperature | 1 |
| 17 | Trace Element Partitioning Between Coexisting Silicate Melts: the Effect of Melt Composition | 1 |
| 18 | Ab-initio molecular dynamic study of phase-D at mantle conditions | 3 |
| 19 | Experimental Determination of High-Pressure Fluid Composition in Equilibrium with Residual Eclogite | 1 |
| 20 | The upper mantle near convergent plate boundaries | 25 |
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.