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.
The Structure of Ferrihydrite, a Nanocrystalline Material
2007757 citationsLars Ehm, Sytle M. Antao et al.profile →
Elasticity of α-Cristobalite: A Silicon Dioxide with a Negative Poisson's Ratio
1992419 citationsDonald J. Weidner, John B. Parise et al.profile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
cites ·
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Countries citing papers authored by John B. Parise
Since
Specialization
Citations
This map shows the geographic impact of John B. Parise'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 B. Parise with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites John B. Parise more than expected).
This network shows the impact of papers produced by John B. Parise. 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 B. Parise. The network helps show where John B. Parise may publish in the future.
Co-authorship network of co-authors of John B. Parise
This figure shows the co-authorship network connecting the top 25 collaborators of John B. Parise.
A scholar is included among the top collaborators of John B. Parise 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 B. Parise. John B. Parise is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Hurowitz, J. A., John B. Parise, Huiqing Zhong, et al.. (2017). Using Diffraction Peaks in X-Ray Fluorescence Spectra from the Mars 2020 PIXL Instrument for Mineral Phase Identification. Lunar and Planetary Science Conference. 2955.1 indexed citations
Parise, John B., Koichiro Umemoto, Renata M. Wentzcovitch, & Donald J. Weidner. (2004). Post-perovskite transition in NaMgF$_3$. AGUFM. 2004.3 indexed citations
13.
Flynn, G. J., et al.. (2000). Combined X-Ray Diffraction Mineralogical Classification and X-Ray Fluorescence Chemical Analysis of Individual Interplanetary Dust Particles. Lunar and Planetary Science Conference. 1772.2 indexed citations
14.
Benning, Liane G., Christopher L. Cahill, S. M. Clark, H. L. Barnes, & John B. Parise. (1999). Mackinawite Stability at High Temperatures. 7227.3 indexed citations
15.
Chen, Jiuhua, Rui Li, John B. Parise, & Donald J. Weidner. (1996). Letters. Pressure-induced ordering in (Ni,Mg)2SiO4 olivine. American Mineralogist. 81. 1519–1522.34 indexed citations
16.
Parise, John B., et al.. (1994). Pressure-induced H bonding; neutron diffraction study of brucite, Mg(OD) 2 , to 9.3 GPa. American Mineralogist. 79. 193–196.121 indexed citations
17.
Parise, John B., Yanbin Wang, Keiji Kusaba, et al.. (1994). High-pressure crystal chemistry of neighborite, NaMgF3: An angle-dispersive diffraction study using monochromatic synchrotron X-radiation. American Mineralogist. 79. 615–621.25 indexed citations
18.
Northrup, Paul, Kurt Leinenweber, & John B. Parise. (1994). The location of H in the high-pressure synthetic Al2SiO4 (OH)2 topaz analogue. American Mineralogist. 79. 401–404.46 indexed citations
19.
Pacalo, Rosemary E. G. & John B. Parise. (1992). Crystal structure of superhydrous B, a hydrous magnesium silicate synthesized at 1400 degrees C and 20 GPa. American Mineralogist. 77. 681–684.59 indexed citations
20.
FitzGerald, John, John B. Parise, & Ian D.R. Mackinnon. (1986). Average structure of an An 48 plagioclase from the Hogarth Ranges. American Mineralogist. 71. 1399–1408.31 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.