Hit papers significantly outperform the citation benchmark for their cohort. A paper qualifies
if it has ≥500 total citations, achieves ≥1.5× the top-1% citation threshold for papers in the
same subfield and year (this is the minimum needed to enter the top 1%, not the average
within it), or reaches the top citation threshold in at least one of its specific research
topics.
Sulfates in Martian Layered Terrains: The OMEGA/Mars Express View
2005772 citationsA. Gendrin, N. Mangold et al.profile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
cites ·
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This map shows the geographic impact of C. Quantin'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 C. Quantin with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites C. Quantin more than expected).
This network shows the impact of papers produced by C. Quantin. 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 C. Quantin. The network helps show where C. Quantin may publish in the future.
Co-authorship network of co-authors of C. Quantin
This figure shows the co-authorship network connecting the top 25 collaborators of C. Quantin.
A scholar is included among the top collaborators of C. Quantin 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 C. Quantin. C. Quantin is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Flahaut, J., J. L. Bishop, S. Silvestro, et al.. (2017). Hydrothermal Alteration on Mars Compared to the Italian Solfatara. Lunar and Planetary Science Conference. 2071.1 indexed citations
3.
Quantin, C., et al.. (2016). Oxia Planum: A Clay-Laden Landing Site Proposed for the ExoMars Rover Mission: Aqueous Mineralogy and Alteration Scenarios. Lunar and Planetary Science Conference. 2064.24 indexed citations
4.
Quantin, C., P. Thollot, Joel Davis, et al.. (2016). Oxia Planum — The Landing Site for ExoMars 2018. LPI. 2863.12 indexed citations
5.
Werner, Stéphanie C., О. П. Попова, C. Quantin, & W. K. Hartmann. (2015). The smallest crater production size-frequency distribution on Mars. EGU General Assembly Conference Abstracts. 10011.1 indexed citations
6.
Flahaut, J., J. L. Bishop, Frank Fueten, et al.. (2014). New Hydrated Phase Detections in Valles Marineris: Insights into the Canyon's Aqueous History. LPICo. 1791. 1411.2 indexed citations
7.
Ody, A., F. Poulet, C. Quantin, et al.. (2014). Candidate Source Regions for SNC Meteorites on Mars. LPICo. 1791. 1227.1 indexed citations
8.
Ody, A., F. Poulet, J. P. Bibring, et al.. (2013). Search for Spectral Analogue Sites of Martian Meteorites Using NIR Data. Lunar and Planetary Science Conference. 2265.1 indexed citations
9.
Bultel, B., C. Quantin, M. Andréani, & H. Clénet. (2013). A new CRISM data analysis tool for the detection of miscellaneous alteration phases. EPSC.1 indexed citations
10.
Clénet, H., C. Quantin, M. Andréani, et al.. (2012). Noachian Crust Composition and Early Alteration Processes in the Vicinity of Valles Marineris as seen from the Central Peaks of Impact Craters. LPICo. 1680. 7026.1 indexed citations
11.
Quantin, C., et al.. (2011). Size frequency distribution of small craters on the Moon. epsc. 2011. 808.1 indexed citations
12.
Werner, Stéphanie C., Alessandro Morbidelli, C. Quantin, W. F. Bottke, & S. Marchi. (2011). Timing of the early geological evolution on Moon and Mars. 2011. 1180.1 indexed citations
13.
Clénet, H., C. Quantin, J. Flahaut, et al.. (2011). Compositional diversity of mafic rocks in the vicinity of Valles Marineris, Mars, using Modified Gaussian Model. Lunar and Planetary Science Conference. 2011(1608). 1674.4 indexed citations
14.
Deit, L. Le, J. Flahaut, C. Quantin, & Pascal Allemand. (2010). Geological Setting of Different Phyllosilicate-rich Deposits Exposed on the Surrounding Plateaus and in the Walls of Valles Marineris, Mars. Lunar and Planetary Science Conference. 1146.1 indexed citations
15.
Flahaut, J., C. Quantin, & Pascal Allemand. (2009). Geology and Mineralogy of the Interior Layered Deposits in Capri/Eos Chasma (Mars), Based on CRISM and HiRiSE Data. Lunar and Planetary Science Conference. 1639.1 indexed citations
16.
Weitz, C. M., E. Z. Noe Dobrea, R. M. E. Williams, et al.. (2009). MRO Observations of Fluvial Features, Sulfates, and Other Landforms in the Melas Chasma Basin. Lunar and Planetary Science Conference. 1874.2 indexed citations
17.
Mangold, N., A. Gendrin, B. Gondet, et al.. (2008). Mineralogy of West Tithonium-Noctis Labyrinthus, Mars: Putative Volcanism on Noctis Canyons Floors. elib (German Aerospace Center). 1592.1 indexed citations
18.
Quantin, C., A. Gendrin, N. Mangold, et al.. (2006). Stratigraphy and Elevation Distribution of Sulfate Deposits in Valles Marineris. elib (German Aerospace Center). 2046.3 indexed citations
19.
Masson, Ph., et al.. (2005). HRSC/MEX Analysis of Valley Networks in Echus Chasma Plateau and in Aeolis Region. 36th Annual Lunar and Planetary Science Conference. 1340.2 indexed citations
20.
Mangold, N., V. Ansan, & C. Quantin. (2004). Martian valley networks observed with THEMIS data: New evidence for surface runoff. 35. 1688.1 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.