This map shows the geographic impact of R. E. Kronyak'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 R. E. Kronyak with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites R. E. Kronyak more than expected).
This network shows the impact of papers produced by R. E. Kronyak. 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 R. E. Kronyak. The network helps show where R. E. Kronyak may publish in the future.
Co-authorship network of co-authors of R. E. Kronyak
This figure shows the co-authorship network connecting the top 25 collaborators of R. E. Kronyak.
A scholar is included among the top collaborators of R. E. Kronyak 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 R. E. Kronyak. R. E. Kronyak is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Rogers, A. D., et al.. (2019). Thermal Inertia and Conductivity Measurements of Mars Analog Rock Samples. 2089. 6337.1 indexed citations
9.
Sun, V. Z., Katie Stack, M. Nachon, et al.. (2018). Late-stage diagenesis in the Murray Formation, Gale Crater, Mars: evidence from diverse concretion morphologies. Lunar and Planetary Science Conference. 1587.1 indexed citations
10.
Yen, A. S., R. Gellert, L. M. Thompson, et al.. (2018). Mobility of Potassium-Rich Fluids on Mars: Implications for Diagenesis. Lunar and Planetary Science Conference. 2690.1 indexed citations
11.
Kronyak, R. E., et al.. (2018). Formation of Fracture Networks in the Siccar Point Group: Implications for Timing of Post-Depositional Fluid Flow in Gale Crater, Mars. Lunar and Planetary Science Conference. 1371.2 indexed citations
Kronyak, R. E., Linda C. Kah, Christopher M. Fedo, et al.. (2017). Capping Units of the Murray Formation, Gale Crater, Mars: Salsberry Peak as a Pre-Stimson Formation Caprock. LPI. 1523.1 indexed citations
14.
Nachon, M., D. Y. Sumner, Salvador Borges, et al.. (2017). Stratigraphic distribution of veins in the Murray and Stimson formations, Gale crater, Mars: Implications for ancient groundwater circulation. AGUFM. 2017.
Kah, Linda C., R. E. Kronyak, Jason Van Beek, et al.. (2015). Diagenetic Crystal Clusters and Dendrites, Lower Mount Sharp, Gale Crater. Lunar and Planetary Science Conference. 1901.6 indexed citations
17.
Kronyak, R. E., Linda C. Kah, D. L. Blaney, et al.. (2015). Garden City Vein Complex, Gale Crater, Mars: Implications for Late Diagenetic Fluid Flow. 2015 AGU Fall Meeting. 2015.1 indexed citations
18.
Kah, Linda C., R. E. Kronyak, Jason Van Beek, et al.. (2015). Late Diagenetic Cements in the Murray Formation, Gale Crater, Mars: Implications for Postdepositional Fluid Flow. AGU Fall Meeting Abstracts. 2015.2 indexed citations
19.
Blaney, D. L., F. J. Calef, L. Le Deit, et al.. (2015). Chemo-stratigraphy at the Pahrump outcrop and Garden City Vein Complex in Gale Crater using ChemCam.. European Planetary Science Congress.
20.
Kronyak, R. E., Linda C. Kah, M. Nachon, et al.. (2015). Distribution of Mineralized Veins from Yellowknife Bay to Mount Sharp, Gale Crater, Mars: Insight from Textural and Compositional Variation. LPI. 1903.6 indexed citations
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.