Diego A. Kietzmann
About
In The Last Decade
Diego A. Kietzmann
61 papers receiving 820 citations
Peers
Comparison fields: 5 of 37
- Paleontology 533
- Atmospheric Science 338
- Earth-Surface Processes 337
- Geophysics 328
- Mechanics of Materials 256
Countries citing papers authored by Diego A. Kietzmann
This map shows the geographic impact of Diego A. Kietzmann'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 Diego A. Kietzmann with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Diego A. Kietzmann more than expected).
Fields of papers citing papers by Diego A. Kietzmann
This network shows the impact of papers produced by Diego A. Kietzmann. 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 Diego A. Kietzmann. The network helps show where Diego A. Kietzmann may publish in the future.
Co-authorship network of co-authors of Diego A. Kietzmann
This figure shows the co-authorship network connecting the top 25 collaborators of Diego A. Kietzmann. A scholar is included among the top collaborators of Diego A. Kietzmann 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 Diego A. Kietzmann. Diego A. Kietzmann 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 | 1 | |
| 4 | 1 | |
| 5 | 0 | |
| 6 | 2 | |
| 7 | 1 | |
| 8 | 1 | |
| 9 | 10 | |
| 10 | 16 | |
| 11 | Palaxius chosmalalensis n. isp., a new crustacean microcoprolite from the Lower Cretaceous of Argentina and new criteria for the classification of ichnospecies of Palaxius | 0 |
| 12 | TOWARDS A MULTIDISCIPLINARY CHRONOSTRATIGRAPHIC CALIBRATION OF THE JURASSIC-CRETACEOUS TRANSITION IN THE NEUQUÉN BASIN | 9 |
| 13 | EVOLUCIÓN PALEOAMBIENTAL DE LA FORMACIÓN REMOREDO (JURÁSICO INFERIOR) EN EL DEPOCENTRO MALARGÜE, CUENCA NEUQUINA SURMENDOCINA | 3 |
| 14 | 23 | |
| 15 | 37 | |
| 16 | Las tempestitas peloidales de la formación Vaca Muerta (Tithoniano-Valanginiano) en el sector surmendocino de la Cuenca Neuquina, Argentina | 12 |
| 17 | Nanofósiles calcáreos de la Formación Vaca Muerta (Tithoniano inferior- Valanginiano inferior) en la región sudoccidental de la provincia de Mendoza, Argentina | 4 |
| 18 | Amonoideos y nanofósiles calcáreos del Tithoniano de la Formación Vaca Muerta en Arroyo Durazno, centro-oeste de Mendoza, Argentina | 2 |
| 19 | Microcrinoideos saccocómidos en el Tithoniano de la Cuenca Neuquina. ¿Una presencia inesperada fuera de la región de influencia directa del Tethys? | 17 |
| 20 | FACIES Y MICROFACIES DE LA RAMPA TITHONIANA- BERRIASIANA DE LA CUENCA NEUQUINA (FORMACIÓN VACA MUERTA) EN LA SECCIÓN DEL ARROYO LONCOCHE - MALARGÜE, PROVINCIA DE MENDOZA | 35 |
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.