M. J. Holdaway
About
In The Last Decade
M. J. Holdaway
40 papers receiving 3.3k citations
Hit Papers
Peers
Comparison fields: 5 of 61
- Geophysics 3.4k
- Artificial Intelligence 1.1k
- Geochemistry and Petrology 414
- Biomaterials 377
- Atmospheric Science 289
Countries citing papers authored by M. J. Holdaway
This map shows the geographic impact of M. J. Holdaway'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 M. J. Holdaway with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites M. J. Holdaway more than expected).
Fields of papers citing papers by M. J. Holdaway
This network shows the impact of papers produced by M. J. Holdaway. 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 M. J. Holdaway. The network helps show where M. J. Holdaway may publish in the future.
Co-authorship network of co-authors of M. J. Holdaway
This figure shows the co-authorship network connecting the top 25 collaborators of M. J. Holdaway. A scholar is included among the top collaborators of M. J. Holdaway 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 M. J. Holdaway. M. J. Holdaway is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 476 | |
| 2 | A reevaluation of the stability relations of andalusite: Thermochemical data and phase diagram for the aluminum silicates | 174 |
| 3 | Staurolite end-member molar volumes determined from unit-cell measurements of natural specimens | 3 |
| 4 | Stable isotope systematics of coexisting biotite and muscovite in high-grade pelitic rocks of southwestern Maine | 2 |
| 5 | A new perspective on staurolite crystal chemistry: Use of stoichiometric and chemical end-members for a mole fraction model | 21 |
| 6 | Rock pressures vs. fluid pressure as a controlling influence on mineral stability; an example from New Mexico | 15 |
| 7 | 32 | |
| 8 | Devonian and Carboniferous metamorphism in west-central Maine; the muscovite-almandine geobarometer and the staurolite problem revisited | 108 |
| 9 | A model for the crystal chemistry of staurolite | 59 |
| 10 | H content of staurolite as determined by H extraction line and ion microprobe | 52 |
| 11 | 69 | |
| 12 | 53 | |
| 13 | Metamorphic petrology, mineral equilibria, and polymetamorphism in the Augusta Quadrangle, South-central Maine | 48 |
| 14 | Chemical formulae and activity models for biotite, muscovite, and chlorite applicable to pelitic metamorphic rocks | 27 |
| 15 | 30 | |
| 16 | A brief description of geological and geophysical exploration of the Marysville geothermal area | 2 |
| 17 | Stability of andalusite and the aluminum silicate phase diagram breakdown → | 1133 |
| 18 | 26 | |
| 19 | Basic regional metamorphic rocks in part of the Klamath Mountains, Northern California | 23 |
| 20 | 37 |
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.