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.
The Global Topography of Mars and Implications for Surface Evolution
1999685 citationsDavid E. Smith, M. T. Zuber et al.profile →
Internal Structure and Early Thermal Evolution of Mars from Mars Global Surveyor Topography and Gravity
2000432 citationsM. T. Zuber, Sean C. Solomon et al.profile →
Citations per year, relative to P. J. McGovern P. J. McGovern (= 1×)
peers
E. R. Stofan
Countries citing papers authored by P. J. McGovern
Since
Specialization
Citations
This map shows the geographic impact of P. J. McGovern'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 P. J. McGovern with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites P. J. McGovern more than expected).
This network shows the impact of papers produced by P. J. McGovern. 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 P. J. McGovern. The network helps show where P. J. McGovern may publish in the future.
Co-authorship network of co-authors of P. J. McGovern
This figure shows the co-authorship network connecting the top 25 collaborators of P. J. McGovern.
A scholar is included among the top collaborators of P. J. McGovern 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 P. J. McGovern. P. J. McGovern is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Öhman, T., G. Y. Kramer, & P. J. McGovern. (2016). Geomorphologic Sketch Mapping of a Fresh Lunar Crater Eimmart A. Lunar and Planetary Science Conference. 1948.1 indexed citations
3.
McGovern, P. J., et al.. (2014). Olivine Exposures on the Moon: Origins and Mechanisms of Transport to the Lunar Surface. Lunar and Planetary Science Conference. 1564.3 indexed citations
4.
Kiefer, W. S., P. J. McGovern, J. C. Andrews‐Hanna, et al.. (2014). The Contribution of Impact Melt Sheets to Lunar Impact Basin Gravity Anomalies. LPI. 2831.1 indexed citations
5.
McGovern, P. J., W. S. Kiefer, G. Y. Kramer, et al.. (2013). Impact-Generated Loading and Lithospheric Stress Gradients at Lunar Impact Basins: Implications for Maria Emplacement Scenarios. Lunar and Planetary Science Conference. 3055.3 indexed citations
6.
McGovern, P. J.. (2012). An Intrusive Origin for Lunar Mascons: Magma Ascent Theory, Gravitational Signatures, and Tests for GRAIL. LPI. 2937.1 indexed citations
7.
McGovern, P. J., et al.. (2011). The Development of Giant Radiating Dike Swarms on Venus from Coupled Mechanical Models. LPI. 2783.1 indexed citations
8.
Kiefer, W. S., et al.. (2011). THERMAL EVOLUTION OF LARGE LUNAR IMPACT BASINS: IMPLICATIONS FOR BASIN COMPENSATION AND THE DURATION OF THE LUNAR CATACLYSM. Lunar and Planetary Science Conference. 2349.
9.
McGovern, P. J., et al.. (2011). Teaching Res Publica and Individual Rights in the First-Year Political Science Course. SSRN Electronic Journal.1 indexed citations
10.
Hurwitz, D. M., et al.. (2007). A Revised Simple Elastic Model of Magma Reservoir Failure Beneath a Volcanic Edifice. Lunar and Planetary Science Conference. 1220.1 indexed citations
11.
McGovern, P. J., et al.. (2006). Structure and Evolution of the Olympus Mons Volcanic Edifice and Basal Escarpment, Mars. LPI. 2329.2 indexed citations
12.
McGovern, P. J. & T. R. Watters. (2004). Loading-induced Stresses near the Martian Hemispheric Dichotomy Boundary. Lunar and Planetary Science Conference. 2148.1 indexed citations
13.
Ruíz, Javier, et al.. (2004). The early thermal and magnetic state of Terra Cimmeria, southern highlands of Mars. Lunar and Planetary Science Conference. 1161.1 indexed citations
14.
McGovern, P. J., et al.. (2004). The Olympus Mons Aureole Deposits: New Evidence for a Flank-Failure Origin. Lunar and Planetary Science Conference. 1980.1 indexed citations
15.
Stepinski, T. F., et al.. (2003). Martian Geomorphology from Statistics of Drainage Networks. Lunar and Planetary Science Conference. 1642.1 indexed citations
16.
Stepinski, T. F., Margarita Marinova, P. J. McGovern, & S. M. Clifford. (2002). The Fractal Characteristics of Martian Drainage Basins: Implications for the Timing, Intensity, and Duration of Rainfall. LPI. 1347.1 indexed citations
17.
McGovern, P. J., Sean C. Solomon, David E. Smith, et al.. (2001). Gravity/Topography Admittances and Lithospheric Evolution on Mars: The Importance of Finite-Amplitude Topography. Lunar and Planetary Science Conference. 1804.7 indexed citations
18.
McGovern, P. J., et al.. (1999). Extension and Volcanic Loading at Alba Patera: Insights from MOLA Observations and Loading Models. Lunar and Planetary Science Conference. 1697.5 indexed citations
19.
Bulmer, M. H. & P. J. McGovern. (1999). Emplacement Kinematics of the Northern Olympus Mons Aureole Deposit. Lunar and Planetary Science Conference. 2016.2 indexed citations
20.
McGovern, P. J. & Sean C. Solomon. (1992). Estimates of elastic plate thicknesses beneath large volcanos on Venus. 789. 68.2 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.