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.
Ti-V plots and the petrogenesis of modern and ophiolitic lavas
Countries citing papers authored by John W. Shervais
Since
Specialization
Citations
This map shows the geographic impact of John W. Shervais'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 John W. Shervais with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites John W. Shervais more than expected).
Fields of papers citing papers by John W. Shervais
This network shows the impact of papers produced by John W. Shervais. 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 John W. Shervais. The network helps show where John W. Shervais may publish in the future.
Co-authorship network of co-authors of John W. Shervais
This figure shows the co-authorship network connecting the top 25 collaborators of John W. Shervais.
A scholar is included among the top collaborators of John W. Shervais 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 John W. Shervais. John W. Shervais is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Shervais, John W., Marguerite Godard, Jeffrey G. Ryan, et al.. (2017). Chemostratigraphy of Subduction Initiation: Boninite and Forearc Basalt from IODP Expedition 352. RUNE (Research UNE). 3608.1 indexed citations
7.
Kessler, James, et al.. (2017). Predicting Uniaxial Compressive Strength From Empirical Relationships Between Ultrasonic P-Wave Velocities, Porosity, and Core Measurements in a Potential Geothermal Reservoir, Snake River Plain, Idaho. OSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information).2 indexed citations
8.
Potter, Katherine E., John W. Shervais, Duane E. Champion, Bob Duncan, & Eric H. Christiansen. (2012). Project Hotspot: Temporal Compositional Variation in Basalts of the Kimama Core and Implications for Magma Source Evolution, Snake River Scientific Drilling Project, Idaho. AGU Fall Meeting Abstracts. 2012.2 indexed citations
9.
Christiansen, Eric H., et al.. (2012). Source and Crystallization Characteristics of Basalts in the Kimama core: Project Hotspot Snake River Scientific Drilling Project, Idaho. AGU Fall Meeting Abstracts. 2012.2 indexed citations
10.
Choi, Sung Hi, John W. Shervais, & Samuel B. Mukasa. (2008). Supra-subduction and abyssal mantle peridotites of the Coast Range ophiolite, California: Initiation of Franciscan subduction along a large-offset fracture zone. EGU General Assembly Conference Abstracts. 72(12). 3928.1 indexed citations
11.
Davis, Owen, et al.. (2006). Neogene Palynology of the Snake River Plain: Climate Change and Volcanic Effects.. AGU Fall Meeting Abstracts. 2006.1 indexed citations
12.
Shervais, John W. & J. J. McGee. (1998). Magma Mixing in the Petrogenesis Alkali Suite Anorthosites: Reverse Zoning in Plagioclase, 14305,303. LPI. 1706.1 indexed citations
13.
Shervais, John W. & J. J. McGee. (1997). KREEP in the Western Lunar Highlands: an Ion Microprobe Study of Alkali and MG Suite Cumulates from the Apollo 12 and 14 Sites. Lunar and Planetary Science Conference. 1301.1 indexed citations
14.
Shervais, John W.. (1994). Ion Microprobe Studies of Lunar Highland Cumulate Rocks: Preliminary Results. LPI. 1265.4 indexed citations
15.
Shervais, John W. & Scott K. Vetter. (1991). Auto-Metasomatism of the Western Lunar Highlands: Result of Closed System Fraction and Mobilization of a KREEPy Trapped Liquid. Lunar and Planetary Science Conference. 22. 1237.3 indexed citations
16.
Shervais, John W., L. A. Taylor, & R. L. Korotev. (1985). Petrology and Mineral Chemistry of Some African Eclogites and the Evolution of Sub-Continental Mantle and Continental Crust. Lunar and Planetary Science Conference. 769–770.3 indexed citations
17.
Shervais, John W., L. A. Taylor, & J. C. Laul. (1984). Very High Potassium (vhk) Basalt: a New Type of Aluminous Mare Basalt from Apollo 14. LPI. 768–769.2 indexed citations
18.
Shervais, John W. & L. A. Taylor. (1983). Texturally-Pristine Clasts from Apollo 14: Implications for Igneous Processes. LPI. 698–699.2 indexed citations
19.
Shervais, John W., L. A. Taylor, & E. Jarosewich. (1983). The Maryville Meteorite, Tennessee: A 1983 Fall of an L6 Chondrite. Metic. 18. 394.1 indexed citations
20.
Shervais, John W. & L. A. Taylor. (1983). Micrographic Granite: More from Apollo 14. LPI. 696–697.3 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.