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.
Trace element fractionation and the origin of tholeiitic and alkaline magma types
1968851 citationsP. W. GastGeochimica et Cosmochimica Actaprofile →
Citations per year, relative to P. W. Gast P. W. Gast (= 1×)
peers
C. C. Schnetzler
Countries citing papers authored by P. W. Gast
Since
Specialization
Citations
This map shows the geographic impact of P. W. Gast'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 P. W. Gast with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites P. W. Gast more than expected).
This network shows the impact of papers produced by P. W. Gast. 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 P. W. Gast. The network helps show where P. W. Gast may publish in the future.
Co-authorship network of co-authors of P. W. Gast
This figure shows the co-authorship network connecting the top 25 collaborators of P. W. Gast.
A scholar is included among the top collaborators of P. W. Gast 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 P. W. Gast. P. W. Gast is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
All Works
20 of 20 papers shown
1.
Nyquist, L. E., N. J. Hubbard, P. W. Gast, et al.. (1973). Rb-Sr systematics for chemically defined Apollo 15 and 16 materials. Lunar Science Conference. 4. 1823.54 indexed citations
2.
Hubbard, N. J., P. W. Gast, L. E. Nyquist, et al.. (1973). Lunar rock types - The role of plagioclase in non-mare and highland rock types. Lunar Science Conference. 4. 1297.42 indexed citations
3.
Bansal, B. M., P. W. Gast, N. J. Hubbard, et al.. (1973). Lunar Rock Types. Lunar and Planetary Science Conference. 4. 48.8 indexed citations
4.
Gast, P. W.. (1973). Lunar Magmatism in Time and Space. Lunar and Planetary Science Conference. 4. 275.1 indexed citations
5.
Hubbard, N. J., P. W. Gast, J. M. Rhodes, et al.. (1972). Nonmare basalts: Part II. 3. 1161.35 indexed citations
6.
Nyquist, L. E., P. W. Gast, & Stan E. Church. (1972). Rb-Sr Relationships for Some Chemically Defined Lunar Materials. Lunar and Planetary Science Conference. 3. 584.1 indexed citations
7.
Nyquist, L. E., N. J. Hubbard, P. W. Gast, et al.. (1972). Rb-Sr systematics for chemically defined Apollo 14 breccias. Lunar and Planetary Science Conference Proceedings. 3. 1515.13 indexed citations
8.
Gast, P. W., et al.. (1972). Evidence for Initial Chemical Layering of the Moon. LPI. 3. 289.7 indexed citations
McConnell, Robert K. & P. W. Gast. (1972). Lunar thermal history revisited. Earth Moon and Planets. 5(1-2). 41–51.25 indexed citations
11.
Gast, P. W. & R. T. Giuli. (1972). Density of the lunar interior. Earth and Planetary Science Letters. 16(2). 299–305.14 indexed citations
12.
Hubbard, N. J., L. E. Nyquist, H. Wiesmann, et al.. (1971). Chemical Composition of Lunar Anorthosites and Their Parent Liquids. LPI. 3. 404.1 indexed citations
Gast, P. W., N. J. Hubbard, & H. Wiesmann. (1970). Chemical composition and petrogenesis of basalts from Tranquillity Base. Geochimica et Cosmochimica Acta Supplement. 1. 1143.65 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.