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 structure of silicate melts: Implications for chemical and physical properties of natural magma
1982543 citationsBjørn O. Mysen, David Virgo et al.profile →
Peers — A (Enhanced Table)
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Countries citing papers authored by Bjørn O. Mysen
Since
Specialization
Citations
This map shows the geographic impact of Bjørn O. Mysen'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 Bjørn O. Mysen with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Bjørn O. Mysen more than expected).
This network shows the impact of papers produced by Bjørn O. Mysen. 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 Bjørn O. Mysen. The network helps show where Bjørn O. Mysen may publish in the future.
Co-authorship network of co-authors of Bjørn O. Mysen
This figure shows the co-authorship network connecting the top 25 collaborators of Bjørn O. Mysen.
A scholar is included among the top collaborators of Bjørn O. Mysen 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 Bjørn O. Mysen. Bjørn O. Mysen is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Roskosz, Mathieu, et al.. (2012). Nitrogen Solubility in Molten Metal and Silicate at High Pressure and Temperature: A First Experimental Approach. LPI. 1497.2 indexed citations
Steele, A., H. E. F. Amundsen, Bjørn O. Mysen, et al.. (2008). An Abiotic Organic Synthesis Mechanism on Mars. Lunar and Planetary Science Conference. 2542.1 indexed citations
6.
Boyd, F. R., Yingwei Fei, C. M. Bertka, & Bjørn O. Mysen. (1999). Mantle petrology : field observations and high-pressure experimentation : a tribute to Francis R. (Joe) Boyd.494 indexed citations
7.
Mysen, Bjørn O., et al.. (1998). The upper mantle near convergent plate boundaries. Reviews in Mineralogy & Geochemistry. 37(1). 97–138.25 indexed citations
8.
Fei, Yingwei, et al.. (1994). Temperature-dependent electron delocalization in (Mg,Fe)SiO 3 perovskite. American Mineralogist. 79. 826–837.45 indexed citations
9.
Mysen, Bjørn O. & John D. Frantz. (1993). Structure of silicate melts at high temperature : in-situ measurements in the system BaO-SiO2 to 1669°C. American Mineralogist. 78. 699–709.70 indexed citations
Mysen, Bjørn O.. (1990). Role of Al in depolymerized, peralkaline aluminosilicate melts in the systems Li 2 O-Al 2 O 3 -SiO 2, Na 2 O-Al 2 O 3 -SiO 2, and K 2 O-Al 2 O 3 -SiO 2. American Mineralogist. 75. 120–134.88 indexed citations
12.
Mysen, Bjørn O. & David Virgo. (1989). Redox equilibria, structure, and properties of Fe-bearing aluminosilicate melts; relationships among temperature, composition, and oxygen fugacity in the system Na 2 O-Al 2 O 3 -SiO 2 -Fe-O. American Mineralogist. 74. 58–76.62 indexed citations
13.
Mysen, Bjørn O. & Ikuo Kushiro. (1988). Condensation, evaporation, melting, and crystallization in the primitive solar nebula; experimental data in the system MgO-SiO 2 -H 2 to 1.0X10 (super -9) bar and 1870 degrees C with variable oxygen fugacity. American Mineralogist. 73(1). 1–19.38 indexed citations
Luth, Robert W., Bjørn O. Mysen, & David Virgo. (1987). Raman spectroscopic study of the solubility behavior of H2 in the system Na2O-Al2O3-SiO2-H2. American Mineralogist. 72. 481–486.38 indexed citations
16.
Wendlandt, Richard F. & Bjørn O. Mysen. (1980). Melting phase relations of natural peridotite +CO 2 as a function of degree of partial melting at 15 and 30 kbar. American Mineralogist. 65. 37–44.61 indexed citations
17.
Mysen, Bjørn O.. (1979). Trace-element partitioning between garnet peridotite minerals and water-rich vapor; experimental data from 5 to 30 kbar. American Mineralogist. 64. 274–287.106 indexed citations
18.
Presnall, D. C., Bjørn O. Mysen, & Ikuo Kushiro. (1978). Correction to the paper Compositional variations of coexisting phases with degree of melting of peridotite in the upper mantle by B. O. Mysen and I. Kushiro. American Mineralogist. 63. 597–597.3 indexed citations
19.
Mysen, Bjørn O. & Ikuo Kushiro. (1977). Compositional variations of coexisting phases with degree of melting of peridotite in the upper mantle. American Mineralogist. 62. 843–856.306 indexed citations
20.
Mysen, Bjørn O.. (1976). Experimental determination of some geochemical parameters relating to conditions of equilibration of peridotite in the upper mantle. American Mineralogist. 61. 677–683.31 indexed citations
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive
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incomplete records, variations in author disambiguation, differences in journal indexing, and
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Rankless may not fully capture the entirety of a scholar's output or impact.