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.
Crystallization thermometers for zircon and rutile
20061.5k citationsE. Bruce Watson, D. A. Wark et al.profile →
TitaniQ: a titanium-in-quartz geothermometer
2006571 citationsD. A. Wark, E. Bruce Watsonprofile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
cites ·
hero ref
This map shows the geographic impact of D. A. Wark'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. A. Wark with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites D. A. Wark more than expected).
This network shows the impact of papers produced by D. A. Wark. 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. A. Wark. The network helps show where D. A. Wark may publish in the future.
Co-authorship network of co-authors of D. A. Wark
This figure shows the co-authorship network connecting the top 25 collaborators of D. A. Wark.
A scholar is included among the top collaborators of D. A. Wark 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. A. Wark. D. A. Wark 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.
Wolff, J. A., et al.. (2006). Petrologic evidence for thermal rejuvenation of crystal mush in the Bandelier Tuff. AGUFM. 2006.1 indexed citations
2.
Wark, D. A., et al.. (2004). Probing Ti in Quartz: Application of the TITANiQ Thermometer to the Bishop Tuff. AGUSM. 2004.6 indexed citations
3.
Wark, D. A., E. Bruce Watson, & Jonathan D. Price. (2001). Permeability of Partially Molten Upper Mantle. 3662.2 indexed citations
4.
Price, Jonathan D., D. A. Wark, & E. Bruce Watson. (2001). Permeability of the Lower Crust and Upper Mantle: Conclusions from Complex Synthetic Rocks. AGU Spring Meeting Abstracts. 2001.2 indexed citations
5.
Wark, D. A., B. Spettel, H. Palme, & A. El Goresy. (1988). Rim Formation by Flash Heating and Metasomatism: Evidence from Vigarano CAI VI-1. LPI. 19. 1230.1 indexed citations
6.
Palme, H. & D. A. Wark. (1988). CV-Chondrites: High Temperature Gas-Solid Equilibrium vs. Parent Body Metamorphism. Lunar and Planetary Science Conference. 19. 897.9 indexed citations
7.
Boynton, W. V. & D. A. Wark. (1987). Origin of CAI Rims--I: The Evidence From the Rare Earth Elements. LPI. 18. 117.5 indexed citations
8.
Boynton, W. V., D. A. Wark, & A. A. Ulyanov. (1986). Trace Elements in Efremovka Fine-Grained Inclusion E14: Evidence for High Temperature, Oxidizing Fractionations in the Solar Nebula. Lunar and Planetary Science Conference. 78–79.6 indexed citations
9.
Wark, D. A.. (1981). Alteration and Metasomatism of Allende Ca-Al Materials. Lunar and Planetary Science Conference. 1145–1147.2 indexed citations
10.
Wark, D. A. & J. F. Lovering. (1980). More Early Solar System Stratigraphy: Coarse-Grained Cai's. LPI. 1208–1210.5 indexed citations
11.
Wark, D. A. & J. F. Lovering. (1980). Second Thoughts about Rims. Lunar and Planetary Science Conference. 1211–1213.2 indexed citations
12.
Lovering, J. F., D. A. Wark, & David K. Sewell. (1979). Refractory Oxide, Titanate, Niobate, and Silicate Accessory Mineralogy of Some Type B Ca-Al Inclusions in the Allende Meteorite. Lunar and Planetary Science Conference. 745.2 indexed citations
13.
Wark, D. A.. (1978). Early Solar System Stratigraphy: the Condensation Sequence from Allende to Chondrites, and the Origin of Chondrules. Lunar and Planetary Science Conference. 1208–1210.6 indexed citations
14.
Wark, D. A. & J. F. Lovering. (1978). Refractory/platinum Metals and Other Opaque Phases in Allende Ca-Al Inclusions. Lunar and Planetary Science Conference. 1214–1216.1 indexed citations
15.
Gatehouse, B. M., Ian E. Grey, J. F. Lovering, & D. A. Wark. (1977). Structural studies of tranquillityite and related synthetic phases.. Lunar and Planetary Science Conference Proceedings. 2. 1831–1838.7 indexed citations
16.
Lovering, J. F. & D. A. Wark. (1975). The lunar crust - chemically defined rock groups and their potassium-uranium fractionation.. Lunar and Planetary Science Conference Proceedings. 2. 1203–1217.5 indexed citations
17.
Lovering, J. F. & D. A. Wark. (1975). The Lunar Crust: Chemically Defined Rock Groups and Their K-U Fractionation. Lunar and Planetary Science Conference. 6. 518.2 indexed citations
18.
Wark, D. A., Allen F. Reid, J. F. Lovering, & A. El Goresy. (1973). Zirconolite (versus zirkelite) in Lunar Rocks. Lunar and Planetary Science Conference. 4. 764.11 indexed citations
19.
Lovering, J. F. & D. A. Wark. (1971). Uranium-enriched phases in Apollo 11 and Apollo 12 basaltic rocks. Lunar and Planetary Science Conference Proceedings. 2. 151.21 indexed citations
20.
Lovering, J. F., D. A. Wark, Allen F. Reid, et al.. (1971). Tranquillityite: A new silicate mineral from Apollo 11 and Apollo 12 basaltic rocks. Lunar and Planetary Science Conference Proceedings. 2. 39.24 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.