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.
Fission-Track Thermochronology and its Application to Geology
2018181 citationsMarco G. Malusà et al.BOA (University of Milano-Bicocca)profile →
Peers — A (Enhanced Table)
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Countries citing papers authored by Marco G. Malusà
Since
Specialization
Citations
This map shows the geographic impact of Marco G. Malusà'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 Marco G. Malusà with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Marco G. Malusà more than expected).
This network shows the impact of papers produced by Marco G. Malusà. 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 Marco G. Malusà. The network helps show where Marco G. Malusà may publish in the future.
Co-authorship network of co-authors of Marco G. Malusà
This figure shows the co-authorship network connecting the top 25 collaborators of Marco G. Malusà.
A scholar is included among the top collaborators of Marco G. Malusà 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 Marco G. Malusà. Marco G. Malusà is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Sun, Weijia, Marco G. Malusà, Liang Zhao, Stéphane Guillot, & Li‐Yun Fu. (2019). Continental subduction without a precursor oceanic slab: geological and geophysical evidence from the Adria-Europe plate boundary zone. EGU General Assembly Conference Abstracts. 5581.1 indexed citations
Agostinetti, Nicola Piana, Simone Salimbeni, Silvia Pondrelli, et al.. (2017). Mantle wedge anisotropy beneath the Western Alps: insights from Receiver Function analysis. EGU General Assembly Conference Abstracts. 12545.1 indexed citations
13.
Malusà, Marco G., Martin Danišík, & Joachim Kuhlemann. (2014). Thermochronological response to rifting and subduction in the Corsica-Sardinia block. EGUGA. 9676.1 indexed citations
14.
Malusà, Marco G.. (2014). Sediment budgets by detrital geochronology and new perspectives in understanding orogenic erosion (solicited). EGUGA. 5655.1 indexed citations
15.
Zanchetta, Stefano, Marco G. Malusà, & Andréa Zanchi. (2013). Pre-collisional development and Cenozoic evolution of the central Southern Alps (N Italy). Rendiconti online della Società Geologica Italiana. 29. 194–197.4 indexed citations
16.
Malusà, Marco G. & Eduardo Garzanti. (2011). Detrital geochronology, mineral fertility and short-term erosion patterns. BOA (University of Milano-Bicocca).1 indexed citations
17.
Zanchetta, Stefano, Andréa Zanchi, Marco G. Malusà, et al.. (2010). New geochronological constrains in the Orobic Alps: a proxy for Late Cretaceous and Eocene compressions in the central Southern Alps. EGU General Assembly Conference Abstracts. 8431.1 indexed citations
18.
Garzanti, Eduardo, Sergio Andò, Marco G. Malusà, & Giovanni Vezzoli. (2010). Understanding bias in provenance studies. EGUGA. 1143.
19.
Crosta, Giovanni B., Federico Agliardi, Paolo Frattini, & Marco G. Malusà. (2009). Deep-seated slope deformations, exhumation and relief in the Alps. BOA (University of Milano-Bicocca). 11. 13437–13437.1 indexed citations
20.
Malusà, Marco G., Massimiliano Zattin, Sergio Andò, Eduardo Garzanti, & Giovanni Vezzoli. (2005). Detrital apatite fission-track ages from the Po sands: Implications for the erosional pattern of the orogenic source areas. BOA (University of Milano-Bicocca). 4. 57–65.1 indexed citations
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive
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incomplete records, variations in author disambiguation, differences in journal indexing, and
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Rankless may not fully capture the entirety of a scholar's output or impact.