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Mantle plume-related magmas typically have higher chalcophile and siderophile element (CSE) contents than mid-ocean ridge basalts (MORB). These differences are often attributed to sulfide-under-saturation of plume-related melts. However, because of e
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Akademický článek
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Autor:
Hübner JM; Earth and Planets Laboratory, Carnegie Institution for Science, Washington, District of Columbia 20015, United States., Shiell TB; Earth and Planets Laboratory, Carnegie Institution for Science, Washington, District of Columbia 20015, United States., Guńka PA; Faculty of Chemistry, Warsaw University of Technology, 00-664 Warsaw, Poland., Tao S; Department of Physics, Rutgers University, Newark, New Jersey 07102, United States., Zhu L; Department of Physics, Rutgers University, Newark, New Jersey 07102, United States., Hansen MF; Earth and Planets Laboratory, Carnegie Institution for Science, Washington, District of Columbia 20015, United States., Bullock ES; Earth and Planets Laboratory, Carnegie Institution for Science, Washington, District of Columbia 20015, United States., Chariton S; Center for Advanced Radiation Sources, The University of Chicago, Chicago, Illinois 60637, United States., Prakapenka VB; Center for Advanced Radiation Sources, The University of Chicago, Chicago, Illinois 60637, United States., Fei Y; Earth and Planets Laboratory, Carnegie Institution for Science, Washington, District of Columbia 20015, United States., Blatov VA; Samara Center for Theoretical Materials Science (SCTMS), Samara State Technical University, Samara 443100, Russia., Proserpio DM; Dipartimento di Chimica, Università degli Studi di Milano, 20133 Milano, Italy., Strobel TA; Earth and Planets Laboratory, Carnegie Institution for Science, Washington, District of Columbia 20015, United States.
Publikováno v:
Journal of the American Chemical Society [J Am Chem Soc] 2024 Jul 31; Vol. 146 (30), pp. 20544-20549. Date of Electronic Publication: 2024 Jul 17.
Autor:
Smith EM; Gemological Institute of America, New York, NY, USA. evan.smith@gia.edu., Shirey SB; Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC, USA., Richardson SH; Department of Geological Sciences, University of Cape Town, Rondebosch, South Africa., Nestola F; Department of Geosciences, University of Padova, Padua, Italy., Bullock ES; Geophysical Laboratory, Carnegie Institution for Science, Washington, DC, USA., Wang J; Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC, USA., Wang W; Gemological Institute of America, New York, NY, USA.
Publikováno v:
Nature [Nature] 2019 Jun; Vol. 570 (7760), pp. E28-E29.
Autor:
Reekie CDJ; Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK. cdjr2@cam.ac.uk., Jenner FE; School of Environment, Earth and Ecosystem Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK., Smythe DJ; Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK., Hauri EH; Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road, Washington, DC, 20015, USA., Bullock ES; Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Road, Washington, DC, 20015, USA., Williams HM; Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK.
Publikováno v:
Nature communications [Nat Commun] 2019 Jan 08; Vol. 10 (1), pp. 82. Date of Electronic Publication: 2019 Jan 08.
Autor:
Smith EM; Gemological Institute of America, New York, NY, USA. evan.smith@gia.edu., Shirey SB; Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC, USA., Richardson SH; Department of Geological Sciences, University of Cape Town, Rondebosch, South Africa., Nestola F; Department of Geosciences, University of Padova, Padua, Italy., Bullock ES; Geophysical Laboratory, Carnegie Institution for Science, Washington, DC, USA., Wang J; Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC, USA., Wang W; Gemological Institute of America, New York, NY, USA.
Publikováno v:
Nature [Nature] 2018 Aug; Vol. 560 (7716), pp. 84-87. Date of Electronic Publication: 2018 Aug 01.
Autor:
Stefanoski S; Geophysical Laboratory, Carnegie Institution of Washington , Washington, D.C. 20015, United States.; Department of Physics, Benedictine University , Lisle, Illinois 60532, United States., Finkelstein GJ; Seismological Laboratory, California Institute of Technology , Pasadena, California 91125, United States., Ward MD; Geophysical Laboratory, Carnegie Institution of Washington , Washington, D.C. 20015, United States., Zeng T; Department of Chemistry, Carleton University , Ottawa, ON K1S5B6, Canada., Wei K; Department of Physics, University of South Florida , Tampa, Florida 33620, United States., Bullock ES; Geophysical Laboratory, Carnegie Institution of Washington , Washington, D.C. 20015, United States., Beavers CM; Advanced Light Source, Lawrence Berkeley National Laboratory , Berkeley, California 94720, United States.; Department of Earth and Planetary Sciences, University of California Santa Cruz , Santa Cruz, California 95064, United States., Liu H; Geophysical Laboratory, Carnegie Institution of Washington , Washington, D.C. 20015, United States., Nolas GS; Department of Physics, University of South Florida , Tampa, Florida 33620, United States., Strobel TA; Geophysical Laboratory, Carnegie Institution of Washington , Washington, D.C. 20015, United States.
Publikováno v:
Inorganic chemistry [Inorg Chem] 2018 Feb 19; Vol. 57 (4), pp. 2002-2012. Date of Electronic Publication: 2018 Feb 05.
Autor:
Zhao Z; Geophysical Laboratory, Carnegie Institution of Washington, Washington, District of Columbia 20015, USA.; State Key Laboratory of Metastable Materials Science and Technology, Yanshan University, Qinhuangdao 066004, China., Zhang H; Geophysical Laboratory, Carnegie Institution of Washington, Washington, District of Columbia 20015, USA., Kim DY; Geophysical Laboratory, Carnegie Institution of Washington, Washington, District of Columbia 20015, USA.; Center for High Pressure Science and Technology Advanced Research, 1690 Cailun Road, Building 6, Pudong, Shanghai 201203, China., Hu W; State Key Laboratory of Metastable Materials Science and Technology, Yanshan University, Qinhuangdao 066004, China., Bullock ES; Geophysical Laboratory, Carnegie Institution of Washington, Washington, District of Columbia 20015, USA., Strobel TA; Geophysical Laboratory, Carnegie Institution of Washington, Washington, District of Columbia 20015, USA.
Publikováno v:
Nature communications [Nat Commun] 2017 Jan 03; Vol. 8, pp. 13909. Date of Electronic Publication: 2017 Jan 03.
Autor:
Smith EM; Gemological Institute of America, New York, NY 10036, USA. evan.smith@gia.edu., Shirey SB; Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC 20015, USA., Nestola F; Department of Geosciences, University of Padova, Padova 35131, Italy., Bullock ES; Geophysical Laboratory, Carnegie Institution for Science, Washington, DC 20015, USA., Wang J; Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC 20015, USA., Richardson SH; Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa., Wang W; Gemological Institute of America, New York, NY 10036, USA.
Publikováno v:
Science (New York, N.Y.) [Science] 2016 Dec 16; Vol. 354 (6318), pp. 1403-1405.