Max Coleman
About
In The Last Decade
Max Coleman
143 papers receiving 7.8k citations
Hit Papers
Peers
Comparison fields: 5 of 155
- Geochemistry and Petrology 2.7k
- Paleontology 2.6k
- Atmospheric Science 2.2k
- Environmental Chemistry 1.8k
- Geophysics 1.8k
Countries citing papers authored by Max Coleman
This map shows the geographic impact of Max Coleman'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 Coleman with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Max Coleman more than expected).
Fields of papers citing papers by Max Coleman
This network shows the impact of papers produced by Max Coleman. 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 Coleman. The network helps show where Max Coleman may publish in the future.
Co-authorship network of co-authors of Max Coleman
This figure shows the co-authorship network connecting the top 25 collaborators of Max Coleman. A scholar is included among the top collaborators of Max Coleman 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 Coleman. Max Coleman 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 | 2 | |
| 4 | Tumbleweed: Wind-Propelled Measurements for Mars | 1 |
| 5 | The trophic structure of fauna and photosynthetic influence at two distinct hydrothermal vent fields on the Mid-Cayman Rise | 1 |
| 6 | 2 | |
| 7 | Sources and Contributions of Oxygen During Microbial Pyrite Oxidation: The Triple Oxygen Isotopes of Sulfate as a Biosignature | 1 |
| 8 | 176 | |
| 9 | Hydrothermal Exploration of the Mid-Cayman Spreading Center: Isolated Evolution on Earth’s Deepest Mid-Ocean Ridge? | 3 |
| 10 | Sulfates on Mars: Comparison with spectral properties of analog sites | 4 |
| 11 | Chemistry and spectroscopy of ironsulfate minerals from Iron Mountain California, U.S.A. | 3 |
| 12 | Abiotic Oxygen Isotope Equilibrium Fractionation Between Sulfite and Water | 18 |
| 13 | Chemical and Isotopic Characterization of Waters in Rio Tinto, Spain, Shows Possible Origin of the Blueberry Haematite Nodules in Meridiani Planum, Mars | 2 |
| 14 | Chlorine isotope composition of trace water in produced oil to characterise production from fracture or matrix in a chalk reservoir | 2 |
| 15 | Palaeoenvironmental conditions of hardgrounds formation in the Late Turonian-Coniacian of Mangyshlak Mountains, Western Kazakhstan | 10 |
| 16 | Review of community based offender programs | 1 |
| 17 | Cyanobacterial key to the genesis of micritic and peloidal limestones in ancient seas | 109 |
| 18 | 88 | |
| 19 | 219 | |
| 20 | Lead isotope variation in the Tynagh, Silvermines and Navan base-metal deposits, Ireland | 16 |
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.