Micro- and nano-inclusions in a superdeep diamond from São Luiz, Brazil


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We report cloudy micro- and nano-inclusions in a superdeep diamond from São-Luiz, Brazil which contains inclusions of ferropericlase (Mg, Fe)O and former bridgmanite (Mg, Fe)SiO3 and ringwoodite (Mg, Fe)2SiO4. Field emission-SEM and TEM observations showed that the cloudy inclusions were composed of euhedral micro-inclusions with grain sizes ranging from tens nanometers to submicrometers. Infrared absorption spectra of the cloudy inclusions showed that water, carbonate, and silicates were not major components of these micro- and nano-inclusions and suggested that the main constituent of the inclusions was infrared-inactive. Some inclusions were suggested to contain material with lower atomic numbers than that of carbon. Mineral phase of nano- and micro-inclusions is unclear at present. Microbeam X-ray fluorescence analysis clarified that the micro-inclusions contained transition metals (Cr, Mn, Fe, Co, Ni, Cu, Zn) possibly as metallic or sulfide phases. The cloudy inclusions provide an important information on the growth environment of superdeep diamonds in the transition zone or the lower mantle.

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Hiroyuki Kagi

Geochemical Research Center, Graduate School of Science

编辑信件的主要联系方式.
Email: kagi@eqchem.s.u-tokyo.ac.jp
日本, Hongo 7-3-1, Tokyo, 113-0033

Dmitry Zedgenizov

V.S. Sobolev Institute of Geology and Mineralogy; Novosibirsk State University

Email: kagi@eqchem.s.u-tokyo.ac.jp
俄罗斯联邦, Koptyuga pr. 3, Novosibirsk, 630090; Pirogova st. 2, Novosibirsk, 630090

Hiroaki Ohfuji

Geodynamics Research Center

Email: kagi@eqchem.s.u-tokyo.ac.jp
日本, Bunkyo-cho 2-5, Ehime, 790-8577

Hidemi Ishibashi

Department of Earth Science, Faculty of Science

Email: kagi@eqchem.s.u-tokyo.ac.jp
日本, Ohya 835, Shizuoka, 422-8529

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