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 viscosity of magmatic silicate liquids; a model calculation
1972618 citationsY. Bottinga, D. F. WeillAmerican Journal of Scienceprofile →
Densities of liquid silicate systems calculated from partial molar volumes of oxide components
1970520 citationsY. Bottinga, D. F. WeillAmerican Journal of Scienceprofile →
Partition of Sr, Ba, Ca, Y, Eu2+, Eu3+, and other REE between plagioclase feldspar and magmatic liquid: an experimental study
1975449 citationsM. J. Drake, D. F. WeillGeochimica et Cosmochimica Actaprofile →
Citations per year, relative to D. F. Weill D. F. Weill (= 1×)
peers
J. A. Philpotts
Countries citing papers authored by D. F. Weill
Since
Specialization
Citations
This map shows the geographic impact of D. F. Weill'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 D. F. Weill with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites D. F. Weill more than expected).
This network shows the impact of papers produced by D. F. Weill. 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 D. F. Weill. The network helps show where D. F. Weill may publish in the future.
Co-authorship network of co-authors of D. F. Weill
This figure shows the co-authorship network connecting the top 25 collaborators of D. F. Weill.
A scholar is included among the top collaborators of D. F. Weill 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 D. F. Weill. D. F. Weill is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
McKay, G. A. & D. F. Weill. (1977). KREEP petrogenesis revisited.. Lunar and Planetary Science Conference Proceedings. 2. 2339–2355.82 indexed citations
3.
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
4.
Weill, D. F. & G. A. McKay. (1975). Major and Trace Element Trends During Minor Experiments on the Crystallization of Lunar Melts. Lunar and Planetary Science Conference. 6. 863.1 indexed citations
5.
McKay, G. A. & D. F. Weill. (1975). Petrogenesis of KREEP. Lunar and Planetary Science Conference Proceedings. 2. 2427–2447.66 indexed citations
6.
Weill, D. F. & G. A. McKay. (1975). The partitioning of Mg, Fe, Sr, Ce, Sm, Eu, and Yb in lunar igneous systems and a possible origin of KREEP by equilibrium partial melting. Lunar and Planetary Science Conference Proceedings. 1. 1143–1158.111 indexed citations
7.
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
8.
McKay, G. A., et al.. (1973). The occurrence and origin of schreibersite-kamacite intergrowths in microbreccia 66055. Lunar and Planetary Science Conference Proceedings. 4. 811.6 indexed citations
Grieve, R. A. F., et al.. (1972). Mineralogy and Petrology of Polymict Breccia 14321. Lunar and Planetary Science Conference. 3. 338.2 indexed citations
11.
Bottinga, Y. & D. F. Weill. (1972). The viscosity of magmatic silicate liquids; a model calculation. American Journal of Science. 272(5). 438–475.618 indexed citations breakdown →
Bottinga, Y., R. A. F. Grieve, I. S. McCallum, & D. F. Weill. (1971). Mineralogy-petrology of lunar samples. Microprobe studies of samples 12021 and 12022; viscosity of melts of selected lunar compositions. Lunar and Planetary Science Conference Proceedings. 2. 413.40 indexed citations
14.
Weill, D. F.. (1971). A Mineralogical-Petrological Survey of Apollo 12 Sample 12013 Using Petrographic Microscope and Electron Microprobe Techniques. Lunar and Planetary Science Conference. 2. 263–263.1 indexed citations
15.
Bottinga, Y., M. J. Drake, I. S. McCallum, G. A. McKay, & D. F. Weill. (1971). Mineralogy and petrology of some Apollo 11 igneous rocks. NASA Technical Reports Server (NASA).34 indexed citations
Bottinga, Y., Albert M. Kudo, & D. F. Weill. (1966). Some observations on oscillatory zoning and crystallization of magmatic plagioclase. American Mineralogist. 51. 792–806.107 indexed citations
Weill, D. F.. (1963). Hydrothermal synthesis of andalusite from Kyanite. American Mineralogist. 48. 944–947.2 indexed citations
20.
Weill, D. F. & W. S. Fyfe. (1961). A preliminary note on the relative stability of andalusite, kyanite, and sillimanite. American Mineralogist. 46. 1191–1195.7 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.