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.
Shape of the subducted Rivera and Cocos plates in southern Mexico: Seismic and tectonic implications
This map shows the geographic impact of M. Pardo'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 M. Pardo with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites M. Pardo more than expected).
This network shows the impact of papers produced by M. Pardo. 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 M. Pardo. The network helps show where M. Pardo may publish in the future.
Co-authorship network of co-authors of M. Pardo
This figure shows the co-authorship network connecting the top 25 collaborators of M. Pardo.
A scholar is included among the top collaborators of M. Pardo 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 M. Pardo. M. Pardo is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Comte, D., Marcelo Farías, S. W. Roecker, Daniel Carrizo, & M. Pardo. (2010). Crustal Normal Faulting Triggered by the Mw=8.8 Maule Megathrust Subduction Earthquake in Central Chile. AGU Fall Meeting Abstracts. 2010.2 indexed citations
Sobiesiak, M., et al.. (2007). The seismogenic structure of the Antofagasta subduction zone and future perspectives for the Iquique Local Network (ILN) in northern Chile. AGU Fall Meeting Abstracts. 2007.1 indexed citations
7.
Monfret, Tony, et al.. (2005). Three dimensional P and S wave velocity models in central Chile and western Argentina (31 0 -34 0 S) from local data: No tear between the fiat and steep segments of the Nazca plate.1 indexed citations
8.
Pardo, M., Tony Monfret, E. Vera, Gonzalo Yáñez, & Amy Eisenberg. (2004). Flat-Slab to Steep Subduction Transition Zone in Central Chile-Western Argentina: Body Waves Tomography and State of Stress. AGUFM. 2004.6 indexed citations
9.
Charrier, Reynaldo, Marcelo Farías, D. Comte, & M. Pardo. (2004). Active Tectonic in the Southern Central Andes, a Recent Example: the 28 August, 2004 Shallow Mw=6.5 Earthquake. AGU Fall Meeting Abstracts. 2004.2 indexed citations
10.
Pardo, M., et al.. (2003). The 2002-2003 CHARSME Experiment : Preliminary Results. AGU Fall Meeting Abstracts. 2003.1 indexed citations
11.
Gras-Martí, A., et al.. (2003). Revision of Prerequisites: ICT Tools. Academic exchange quarterly. 7(3). 312.4 indexed citations
12.
Pardo, M., et al.. (2002). Seismotectonic and Body-wave Tomography of Central Chile-nw Argentina Flat-slab Subduction Zone Using Local Earthquakes. EGSGA. 1454.1 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.