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.
USING THERMOCHRONOLOGY TO UNDERSTAND OROGENIC EROSION
2006804 citationsPeter W. Reiners, M. T. Brandonprofile →
The pMELTS: A revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa
Countries citing papers authored by Peter W. Reiners
Since
Specialization
Citations
This map shows the geographic impact of Peter W. Reiners'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 Peter W. Reiners with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Peter W. Reiners more than expected).
Fields of papers citing papers by Peter W. Reiners
This network shows the impact of papers produced by Peter W. Reiners. 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 Peter W. Reiners. The network helps show where Peter W. Reiners may publish in the future.
Co-authorship network of co-authors of Peter W. Reiners
This figure shows the co-authorship network connecting the top 25 collaborators of Peter W. Reiners.
A scholar is included among the top collaborators of Peter W. Reiners 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 Peter W. Reiners. Peter W. Reiners is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Thomson, Stuart N., et al.. (2019). New constraints on the pre-glacial and glacial uplift and incision history of the central Transantarctic Mountains using multiple low-temperature thermochronometers. AGUFM. 2019.1 indexed citations
Zapata, S., et al.. (2012). Separation of the Guajira-Bonaire pair: 65-50Ma exhumation followed by 300 km right-lateral transtensional deformation. Repositorio Institucional UN - Biblioteca Digital.1 indexed citations
9.
Murray, Kendra E., et al.. (2011). Apatite (U-Th)/He Date Dispersion Due to Secondary Grain Boundary Phases: An Example from the Henry Mountains, Utah. AGUFM. 2011.5 indexed citations
10.
Reiners, Peter W., et al.. (2011). Low-T Thermochronology of St. Severin LL6 Chondrite Revealed from Single-Grain Phosphate (U-Th)/He Ages. LPI. 2683.1 indexed citations
Reiners, Peter W., et al.. (2008). Secondary weathering phases and apatite (U-Th)/He ages. Geochimica et Cosmochimica Acta Supplement. 72(12).3 indexed citations
14.
Reiners, Peter W., et al.. (2007). Low-Temperature Thermochronology of Borehole and Surface Samples From the Wind River and Beartooth Laramide Ranges, Wyoming and Montana, USA. AGUFM. 2007.1 indexed citations
Hourigan, J. K., et al.. (2004). Timing of syenite intrusions on the eastern slope of the Sredinnyi Range, Kamchatka: Rate of accretionary structure exhumation. Geochemistry International. 42(2). 131–141.13 indexed citations
18.
Reiners, Peter W.. (2003). (U-Th)/He dating and calibration of low-T thermochronometry. GeCAS. 67(18). 395.2 indexed citations
19.
Ducea, Mihai N., et al.. (2002). Cenozoic plate tectonic history of southwestern Mexico; constraints from low temperature thermochronology. Geotemas ( Madrid ). 137–138.3 indexed citations
20.
Brandon, M. T., Ernesto Abbate, Matthias Bernet, et al.. (2001). Quantifying Exhumation History Across the Northern Apennines. AGU Fall Meeting Abstracts. 2001.1 indexed citations
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive
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Rankless may not fully capture the entirety of a scholar's output or impact.