This map shows the geographic impact of John Casey'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 Casey with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites John Casey more than expected).
This network shows the impact of papers produced by John Casey. 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 Casey. The network helps show where John Casey may publish in the future.
Co-authorship network of co-authors of John Casey
This figure shows the co-authorship network connecting the top 25 collaborators of John Casey.
A scholar is included among the top collaborators of John Casey 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 Casey. John Casey is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Casey, John & John Dewey. (2014). The Relationships of Plate Triple-junction Evolution, Trench-Arc Lengthening, Boninite Generation, and SSZ Spreading Centers to Ophiolite Formation, High-Temperature Soles, and Obduction. 2014 AGU Fall Meeting. 2014.1 indexed citations
6.
Casey, John & John Dewey. (2013). Arc/Forearc Lengthening at Plate Triple Junctions and the Formation of Ophiolitic Soles. EGUGA. 13430.1 indexed citations
7.
Shaulis, Barry, et al.. (2012). Timing of flysch sedimentation in the Ouachita remnant ocean basin: Constraints from U-Pb ages of zircon in subaqueous tuff deposits. AGU Fall Meeting Abstracts. 2012.1 indexed citations
8.
Berkenhagen, Jörg, et al.. (2011). Review of economic data collected in relation to the DCF and harmonisation of sampling strategies (STECF-11-19). OpenAgrar.1 indexed citations
9.
Casey, John, et al.. (2010). The Lowest δ7Li Yet Recorded in MORB Glasses: The Connection with Oceanic Core Complex Formation, Refractory Rutile-bearing Eclogitic Mantle Sources and Melt Supply. AGU Fall Meeting Abstracts. 2010.1 indexed citations
10.
Casey, John & John Dewey. (2009). The Ophiolite Problem, Is It Really a Problem?. AGUFM. 2009.1 indexed citations
11.
Casey, John, et al.. (2008). Isotopic fractionation of Li during cooling of mantle peridotite from Gakkel Ridge. AGUFM. 2008.1 indexed citations
12.
Hoefs, J., Kari M. Cooper, Christine Laverne, et al.. (2007). Lithium and Oxygen Isotopic Composition of the Oceanic Crust formed at a Superfast Spreading Ridge, Hole 1256D. AGUFM. 2007.2 indexed citations
13.
Searle, R. C., C. J. MacLeod, Bramley J. Murton, et al.. (2007). Development of Oceanic Core Complexes on the Mid-Atlantic Ridge at 13-14N: Deep-Towed Geophysical Measurements and Detailed Seafloor Sampling. AGU Fall Meeting Abstracts. 2007.1 indexed citations
Bird, D. E., et al.. (2005). Late Jurassic - Early Cretaceous tectonic reconstructions of the Central and South Atlantic Oceans. AGU Spring Meeting Abstracts. 2005.1 indexed citations
Bird, D. E., et al.. (2001). Geophysical Evidence for a Possible Late Jurassic Mantle Plume in the Gulf of Mexico. AGU Fall Meeting Abstracts. 2001.1 indexed citations
18.
Casey, John, et al.. (2001). Multi-sensory investigation of geoscientific data: adding touch and sound to three-dimentional visualization and modeling.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.