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.
Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets using new thermobarometers for mafic magmas
2009628 citationsCin‐Ty A. Lee, Péter Luffi et al.Earth and Planetary Science Lettersprofile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
cites ·
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This map shows the geographic impact of H. Dalton'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 H. Dalton with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites H. Dalton more than expected).
This network shows the impact of papers produced by H. Dalton. 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 H. Dalton. The network helps show where H. Dalton may publish in the future.
Co-authorship network of co-authors of H. Dalton
This figure shows the co-authorship network connecting the top 25 collaborators of H. Dalton.
A scholar is included among the top collaborators of H. Dalton 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 H. Dalton. H. Dalton is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
All Works
7 of 7 papers shown
1.
Shipp, Stephanie, et al.. (2010). Get Involved in Planetary Science Education and Public Outreach. LPI. 2318.1 indexed citations
2.
Lee, Cin‐Ty A., Péter Luffi, Terry Plank, H. Dalton, & William P. Leeman. (2009). Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets using new thermobarometers for mafic magmas. Earth and Planetary Science Letters. 279(1-2). 20–33.628 indexed citations breakdown →
3.
Lapen, T. J., et al.. (2008). Lu-Hf Age and Isotope Systematics of the Olivine-Phyric Shergottite RBT 04262 and Implications for the Sources of Enriched Shergottites. Lunar and Planetary Science Conference. 2073.10 indexed citations
4.
Dalton, H., T. G. Sharp, & J. R. Holloway. (2007). INVESTIGATION OF THE EFFECTS OF WATER ON A MARTIAN MANTLE COMPOSITION. H. A.. LPI. 2102.4 indexed citations
5.
Dalton, H. & P. R. Christensen. (2006). Investigation of the Extent of the Apollinaris Patera Ash Deposits: Implications for the Origin of the Columbia Hills. LPI. 2430.1 indexed citations
Dalton, H., D. S. Musselwhite, W. S. Kiefer, & A. H. Treiman. (2005). Experimental Petrology of the Basaltic Shergottite Yamato 980459: Implications for the Thermal Structure of the Martian Mantle. 36th Annual Lunar and Planetary Science Conference. 2142.7 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.