Andrzej Kozłowski
About
In The Last Decade
Andrzej Kozłowski
48 papers receiving 468 citations
Peers
Comparison fields: 5 of 51
- Geophysics 341
- Geometry and Topology 119
- Mathematical Physics 109
- Geochemistry and Petrology 106
- Artificial Intelligence 95
Countries citing papers authored by Andrzej Kozłowski
This map shows the geographic impact of Andrzej Kozłowski'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 Andrzej Kozłowski with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Andrzej Kozłowski more than expected).
Fields of papers citing papers by Andrzej Kozłowski
This network shows the impact of papers produced by Andrzej Kozłowski. 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 Andrzej Kozłowski. The network helps show where Andrzej Kozłowski may publish in the future.
Co-authorship network of co-authors of Andrzej Kozłowski
This figure shows the co-authorship network connecting the top 25 collaborators of Andrzej Kozłowski. A scholar is included among the top collaborators of Andrzej Kozłowski 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 Andrzej Kozłowski. Andrzej Kozłowski is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 1 | |
| 2 | Oxygenic bismuth minerals in the NE part of the Karkonosze pluton (West Sudetes, SW Poland) | 3 |
| 3 | 5 | |
| 4 | 4 | |
| 5 | Sphalerite origin in the Olkusz mining district: a fluid inclusion model | 3 |
| 6 | 6 | |
| 7 | FORMATION CONDITIONS OF QUARTZ MINERALIZATION IN THE MYLONITIC ZONES AND ON THE SLICKENSIDE FAULT PLANES IN THE HIGH TATRA GRANITOIDS | 11 |
| 8 | 18 | |
| 9 | Origin of Zn-Pb ores in the Olkusz and Chrzanów districts: A model based on fluid inclusions | 12 |
| 10 | Origin and evolution of the granite/serpentinite reaction zones at Wiry, Lower Silesia | 5 |
| 11 | 3 | |
| 12 | 4 | |
| 13 | Calcium-rich inclusion solutions in fluorite from the Strzegom pegmatites, Lower Silesia | 15 |
| 14 | Melt inclusions in pyroclastic quartz from the Carboniferous deposits of the Holy Cross•Mts, and the problem of magmatic corrosion | 10 |
| 15 | Parent fluids of the zinc and lead ores from the Silesia-Cracow region | 6 |
| 16 | Pneumatolytic and hydrothermal activity in the Karkonosze-Izera block | 19 |
| 17 | Bismuth minerals from the Karkonosze massif | 9 |
| 18 | Tungsten-tin-molybdenum mineralization in the Karkonosze massif | 14 |
| 19 | Mineralizacj.a wolframitowa z okolic Szklarskiej Poręby Huty | 3 |
| 20 | Kwarc pomagmowy masywu strzegomskiego i karkonoskiego; jego środowisko krystalizacji i pierwiastki śladowe | 2 |
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.