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.
Iron-Titanium Oxide Minerals and Synthetic Equivalents
Countries citing papers authored by D. H. Lindsley
Since
Specialization
Citations
This map shows the geographic impact of D. H. Lindsley'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. H. Lindsley with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites D. H. Lindsley more than expected).
This network shows the impact of papers produced by D. H. Lindsley. 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. H. Lindsley. The network helps show where D. H. Lindsley may publish in the future.
Co-authorship network of co-authors of D. H. Lindsley
This figure shows the co-authorship network connecting the top 25 collaborators of D. H. Lindsley.
A scholar is included among the top collaborators of D. H. Lindsley 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. H. Lindsley. D. H. Lindsley 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.
Nekvasil, H., et al.. (2016). Modifying Martian Surface Chemistry: Chlorides as Sublimates from Volcanic Degassing on Mars. Lunar and Planetary Science Conference. 1517.2 indexed citations
2.
Nekvasil, H., et al.. (2015). SIMULATING A MARTIAN FUMAROLE: UNDERSTANDING THE EFFECTS OF A DEGASSING MARTIAN MAGMA ON SURROUNDING ROCK.. LPI. 2305.3 indexed citations
3.
Nekvasil, H., et al.. (2013). Alkali Depletion of the Bulk Moon, is it Required?. Lunar and Planetary Science Conference. 2830.1 indexed citations
4.
McCubbin, F. M., et al.. (2009). Hydrous Magmatism on Mars: A Source for Water on the Ancient Martian Surface and the Current Martian Subsurface?. Lunar and Planetary Science Conference. 2207.2 indexed citations
5.
McCubbin, F. M., H. Nekvasil, & D. H. Lindsley. (2006). Apatite as a Key to Evaluating the Volatile Budget of Martian Magmas: Implications from the Chassigny Meteorite. 37th Annual Lunar and Planetary Science Conference. 1098.2 indexed citations
6.
Tosca, Nicholas J., S. M. McLennan, D. H. Lindsley, & Martin A. A. Schoonen. (2003). Acid-Sulfate Weathering of Synthetic Martian Basalt: The Acid Fog Model Revisited. Lunar and Planetary Science Conference. 1325.17 indexed citations
7.
Davidson, Paula M. & D. H. Lindsley. (1994). Effect of Ca content and SiO 2 activity on augite + olivine equilibria. American Mineralogist. 79. 1123–1124.8 indexed citations
8.
Lindsley, D. H. & Carol D. Frost. (1992). Equilibria among Fe-Ti oxides, pyroxenes, olivine, and quartz; Part I, Theory. American Mineralogist. 77. 987–1003.126 indexed citations
Lindsley, D. H.. (1991). Experimental studies of oxide minerals. Reviews in Mineralogy & Geochemistry. 25(1). 69–106.142 indexed citations
11.
Lindsley, D. H., et al.. (1985). Tetrahedral al in amphibole: a potential thermometer for some mafic rocks. Geol. Soc. Am., Abstr. Programs; (United States). 17.13 indexed citations
12.
Andersen, David J. & D. H. Lindsley. (1984). Application of a Two-Pyroxene Thermometer: Correlation of Apparent Temperature with AL2O3 in Augite. Lunar and Planetary Science Conference. 7–8.2 indexed citations
13.
Mukhopadhyay, Dilip K. & D. H. Lindsley. (1983). Phase relations in the join kirschsteinite (CaFeSiO 4 )-fayalite (Fe 2 SiO 4 ). American Mineralogist. 68. 1089–1094.41 indexed citations
14.
Delano, J. W. & D. H. Lindsley. (1982). Chromium, Nickel, and Titanium Abundances in 74275 Olivines: More Evidence for a High-Pressure Origin of High-Titanium Mare Basalts. Lunar and Planetary Science Conference. 160–161.5 indexed citations
Lindsley, D. H.. (1980). Phase equilibria of pyroxenes at pressures >1 atmosphere. Reviews in Mineralogy & Geochemistry. 7(1). 289–307.32 indexed citations
17.
Gasparik, Tibor & D. H. Lindsley. (1980). Phase equilibria at high pressure of pyroxenes containing monovalent and trivalent ions. Reviews in Mineralogy & Geochemistry. 7(1). 309–339.92 indexed citations
18.
Grove, T. L. & D. H. Lindsley. (1978). Compositional Variation and Origin of Lunar Ultramafic Green Glasses. Lunar and Planetary Science Conference. 430–432.9 indexed citations
19.
Kesson, S. E. & D. H. Lindsley. (1975). The effects of Al/3+/, Cr/3+/, and Ti/3+/ on the stability of armalcolite. Lunar and Planetary Science Conference Proceedings. 1. 911–920.11 indexed citations
20.
Smith, Douglas & D. H. Lindsley. (1971). Stable and metastable augite crystallization trends in a single basalt flow. American Mineralogist. 56. 225–233.58 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.