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.
Carbon and oxygen isotopic composition of selected limestones and fossils
1964616 citationsM. L. Keith, Jon N. WeberGeochimica et Cosmochimica Actaprofile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
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This map shows the geographic impact of Jon N. Weber'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 Jon N. Weber with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Jon N. Weber more than expected).
This network shows the impact of papers produced by Jon N. Weber. 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 Jon N. Weber. The network helps show where Jon N. Weber may publish in the future.
Co-authorship network of co-authors of Jon N. Weber
This figure shows the co-authorship network connecting the top 25 collaborators of Jon N. Weber.
A scholar is included among the top collaborators of Jon N. Weber 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 Jon N. Weber. Jon N. Weber is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Baker, Paul A. & Jon N. Weber. (1975). Coral growth rate: Variation with depth. Physics of The Earth and Planetary Interiors. 10(2). 135–139.22 indexed citations
Henisch, H.K., et al.. (1971). Physical characterization of lunar glasses and fines. Lunar and Planetary Science Conference Proceedings. 2. 2213.6 indexed citations
7.
Weber, Jon N.. (1969). Origin of Concentric Banding in the Spines of the Tropical Echinoid Heterocentrotus. ScholarSpace (University of Hawaii at Manoa).14 indexed citations
8.
Weber, Jon N. & David M. Raup. (1968). Comparison of C 13 /C 12 and O 18 /O 16 in the skeletal calcite of Recent and fossil echinoids. Journal of Paleontology. 42(1). 37–50.13 indexed citations
Weber, Jon N.. (1966). Dehydration of diaspore at water pressures from 15 to 15,000 psi. American Mineralogist. 51. 235–238.2 indexed citations
12.
Weber, Jon N.. (1965). DEHYDROXYLATION OF KOALINITE DICKITE AND HALLOYSITE: HEATS OF REACTION AND KINETICS OF DEITYDRATION AT P(WATER) = 15 PSI. American Mineralogist. 50(7). 1038–1045.16 indexed citations
13.
Weber, Jon N. & Raymond T. Greer. (1965). Dehydration of serpentine: heat of reaction and reaction kinetics at PH2O=1 ATM.. American Mineralogist. 50. 450–464.31 indexed citations
Weber, Jon N., et al.. (1964). Carbon isotopic composition of lacustrine Gastropoda from pond-weed environments. Journal of Paleontology. 38(5). 965–967.4 indexed citations
19.
Weber, Jon N. & M. L. Keith. (1963). Isotopic composition and environmental classification of selected limestones and fossils.53 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.