Vali Memeti
About
In The Last Decade
Vali Memeti
25 papers receiving 474 citations
Peers
Comparison fields: 5 of 26
- Geophysics 472
- Artificial Intelligence 186
- Mechanics of Materials 23
- Atmospheric Science 23
- Paleontology 22
Countries citing papers authored by Vali Memeti
This map shows the geographic impact of Vali Memeti'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 Vali Memeti with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Vali Memeti more than expected).
Fields of papers citing papers by Vali Memeti
This network shows the impact of papers produced by Vali Memeti. 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 Vali Memeti. The network helps show where Vali Memeti may publish in the future.
Co-authorship network of co-authors of Vali Memeti
This figure shows the co-authorship network connecting the top 25 collaborators of Vali Memeti. A scholar is included among the top collaborators of Vali Memeti 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 Vali Memeti. Vali Memeti is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 15 | |
| 2 | 2 | |
| 3 | 65 | |
| 4 | The Late Cretaceous, migrating Jack Main intrusive complex, central Sierra Nevada, CA: Mapping as a powerful tool for unraveling magmatic histories | 1 |
| 5 | 1 | |
| 6 | Schlieren-bound Magmatic Structures Formed by the Unmixing of Granitic Magmas: A Case Study from Pothole Dome, Sierra Nevada | 1 |
| 7 | EXPLORING VOLCANIC-PLUTONIC CONNECTIONS IN THE BONANZA CALDERA, COLORADO | 2 |
| 8 | 12 | |
| 9 | Geochronologic, Isotopic, and Trace Element Constraints on Zircon Recycling in Sierra Crest Intrusive Suites, Sierra Nevada Batholith, USA | 1 |
| 10 | 169 | |
| 11 | Examining the role and relative timing of magma mixing and fractionation in the formation of the Kuna Crest lobe of the Tuolumne batholith, Sierra Nevada, USA | 2 |
| 12 | Thermal models, stable isotopes and cooling ages from the incrementally constructed Tuolumne batholith, Sierra Nevada: why large chambers did exist | 3 |
| 13 | Interpreting Al-in Hornblende and Hbl-Plag thermobarometry results from the Tuolumne batholith and magmatic lobes in conjunction with single mineral element distribution electron microprobe maps | 5 |
| 14 | Examining the role of magma mixing with major and minor element distribution patterns in rock-forming minerals in the Tuolumne batholith, Sierra Nevada, CA | 2 |
| 15 | 19 | |
| 16 | TI: Downward Crustal Flow During Magma Ascent in the Central Sierran Arc | 1 |
| 17 | TI: Size and Longevity of Magma Chambers in the Tuolumne Batholith: A Comparison of Thermal Modeling and Cooling Thermochronology | 8 |
| 18 | Dynamics of a Magma Chamber: Insights Into Time and Length Scales of Internal Processes in the Tuolumne Batholith, CA | 4 |
| 19 | Growth of the Tuolumne Batholith: Zircon Crystallization Temperature, Age and Trace Element Data | 6 |
| 20 | TI: Tracking Down Batholith Construction Through Time Using Lobes From The Tuolumne Batholith, Sierra Nevada, CA. | 1 |
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.