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.
Geochemistry and Mineralogy of Rare Earth Elements
Citations per year, relative to G. A. McKay G. A. McKay (= 1×)
peers
P. C. Hess
Countries citing papers authored by G. A. McKay
Since
Specialization
Citations
This map shows the geographic impact of G. A. McKay'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 G. A. McKay with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites G. A. McKay more than expected).
This network shows the impact of papers produced by G. A. McKay. 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 G. A. McKay. The network helps show where G. A. McKay may publish in the future.
Co-authorship network of co-authors of G. A. McKay
This figure shows the co-authorship network connecting the top 25 collaborators of G. A. McKay.
A scholar is included among the top collaborators of G. A. McKay 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 G. A. McKay. G. A. McKay 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.
Golden, D. C., D. W. Ming, R. V. Morris, et al.. (2003). Morphological Evidence for an Exclusively Inorganic Origin for Magnetite in Martian Meteorite ALH84001. Lunar and Planetary Science Conference. 1970.2 indexed citations
2.
Draper, D. S., D. D. Bogard, C. B. Agee, G. A. McKay, & J. H. Jones. (2002). Merits of a Locality Sample for Accomplishing Mars Exploration Goals: The First Sample Return Mission. AGU Spring Meeting Abstracts. 2002.
3.
Herd, C. D. K., A. H. Treiman, G. A. McKay, & C. K. Shearer. (2002). Implications of Experimental Lithium and Boron Partition Coefficients for the Petrogenesis of Martian Basalts. Meteoritics and Planetary Science Supplement. 37.4 indexed citations
4.
Golden, D. C., D. W. Ming, M. E. Zolensky, et al.. (2002). Morphology of Magnetite Formed Via Thermal Decomposition of Siderite: Implications for Inorganic Formation of Magnetite in Martian Meteorite ALH84001. Meteoritics and Planetary Science Supplement. 37.1 indexed citations
5.
Mikouchi, T., G. A. McKay, & Le Liu. (2000). Experimental Crystallization of the Asuka 881371 (Angrite) Groundmass Composition: Implications for Crystallization Histories of Sahara 99555. Meteoritics and Planetary Science Supplement. 35.4 indexed citations
6.
Golden, D. C., D. W. Ming, C. S. Schwandt, et al.. (2000). Inorganic Formation of Zoned Mg-Fe-Ca Carbonate Globules with Magnetite and Sulfide Rims Similar to Those in Martian Meteorite ALH84001. Lunar and Planetary Science Conference. 1799.3 indexed citations
Schwandt, C. S., G. A. McKay, & G. E. Lofgren. (1999). FESEM Imaging Reveals Previously Unseen Detail and Enhances Interpretations of ALH84001 Carbonate Petrogenesis. 1346.4 indexed citations
9.
Matney, Mark, et al.. (1999). The Use of the Satellite Breakup Risk Assessment Model (SBRAM) to Characterize Collision Risk to Manned Spacecraft.1 indexed citations
10.
Mikouchi, T., G. A. McKay, & M. Miyamoto. (1998). Comparative Mineralogy of Shocked Plagioclase in Martian and Lunar Meteorites. M&PSA. 33.1 indexed citations
11.
McKay, G. A. & G. E. Lofgren. (1997). Carbonates in ALH84001: Evidence for Kinetically Controlled Growth. Lunar and Planetary Science Conference. 921.14 indexed citations
12.
McKay, G. A., T. Mikouchi, & G. E. Lofgren. (1997). Carbonates and Feldspathic Glass in Allan Hills 84001: Additional Complications. M&PSA. 32.3 indexed citations
13.
Mikouchi, T., M. Miyamoto, & G. A. McKay. (1996). Mineralogy and Petrology of New Antarctic Shergottite QUE94201: A Coarse-Grained Basalt With Unusual Pyroxene Zoning. Lunar and Planetary Science Conference. 27. 879.9 indexed citations
14.
Dickinson, T., G. E. Lofgren, & G. A. McKay. (1990). REE Partitioning Between Silicate Liquid and Immiscible Sulfide Liquid: The Origin of the Negative EU Anomaly in Aubrite Sulfides. LPI. 21. 284.5 indexed citations
15.
McKay, G. A.. (1989). Partitioning of rare earth elements between major silicate minerals and basaltic melts. Reviews in Mineralogy & Geochemistry. 21(1). 45–77.147 indexed citations
16.
Colson, R. O., L. A. Taylor, & G. A. McKay. (1986). Predictive Thermodynamic Modeling for Trace Element Partitioning in Magmatic Systems. LPI. 144–145.2 indexed citations
17.
Wooden, Joseph L., L. E. Nyquist, D. D. Bogard, et al.. (1979). Radiometric Ages for the Achondrites Chervony Kut, Governador Valadares and Allan Hills 77005. LPI. 1379–1381.21 indexed citations
18.
McKay, G. A. & D. F. Weill. (1977). KREEP petrogenesis revisited.. Lunar and Planetary Science Conference Proceedings. 2. 2339–2355.82 indexed citations
19.
McKay, G. A. & D. F. Weill. (1976). Application of Major and Trace Element Crystal/Liquid Partitioning to the origin of KREEP. LPI. 7. 527.5 indexed citations
20.
Weill, D. F., et al.. (1974). Modeling the evolution of Sm and Eu abundances during lunar igneous differentiation. Lunar and Planetary Science Conference Proceedings. 2. 1337–1352.25 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.