「silicates」の共起表現一覧(1語右で並び替え)

silicates

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該当件数:35件

  • 09 Silicates and Germanates
  • It is composed of silicates and metals.
  • of pyrite and marcasite along with aluminous silicates and clays.
  • that it is composed of carbon, organic rich silicates and possibly water ice.
  • orphous mixture of uranium minerals, oxides, silicates and hydrates of uranium, derived from the al
  • rs of the family, its surface is composed of silicates and some nickel-iron, and is quite bright.
  • It is composed of silicates and metallic nickel-iron, and may be the cor
  • composition and composed largely of hydrated silicates and organic material.
  • hydrated materials on its surface, abundant silicates, and a thicker regolith than most asteroids.
  • Therefore, at the Earth's surface silicates are converted to carbonate sediments, but th
  • M. Stolper for a report "Densities of Liquid Silicates at High Pressures," Science 30 November 1984
  • al University he began experimental study of silicates at high pressure, and in 1959 demonstrated t
  • lowing: The Action of Sulphurets on Metallic Silicates at High Temperatures; The Relations of the S
  • of two structurally similar earth -alkaline silicates, Ca2SiO4 and Mg2SiO4, respectively.
  • oid and is probably composed of organic rich silicates, carbon and anhydrous silicates.
  • oid and is probably composed of organic-rich silicates, carbon and anhydrous silicates.
  • that they have a composition of organic rich silicates, carbon and anhydrous silicates, possibly wi
  • Characteristics include complex silicates containing zirconium, titanium the rare eart
  • rbonates significantly outpaces formation of silicates, effectively dissipating primordial carbon d
  • indicates the possible presence of hydrated silicates indicating that 135 Hertha should possibly b
  • ognised: inorganic colloids (clay particles, silicates, iron oxy-hydroxides, ...), organic colloids
  • and (the 3-µm absorption feature of hydrated silicates), Lebofsky discovered the first D-type aster
  • netite; the carbonate siderite and iron rich silicates like some garnets.
  • ts a rather complex mixture of chromates and silicates of lead and arsenic.
  • as been expanded to refer to calcium-bearing silicates of any age.
  • f iron oxide; the clay also contains hydrous silicates of aluminum and possibly magnesium.
  • te mineral which consists principally of the silicates of cerium, lanthanum, neodymium, yttrium, be
  • Cl-, F-, CO3- and possibly also SO4-bearing silicates of Na, K, H3O, Ca, Sr, REEs, Mn, Fe, Nb and
  • high level of organic compounds, and rich in silicates, oxides, and sulfides.
  • elatively small proportion of ferromagnesian silicates, such as amphibole, pyroxene, and biotite.
  • Silicates taken in along with food are deposited in th
  • the afwillite, but both formed from calcium silicates through hydration.
  • eated to several hundred degrees; it acts on silicates, titanates, etc., the same way as sulfuric a
  • acive phase transitions in materials such as silicates, which can be described as infinite three-di
  • of other minerals, such as uranyl oxides and silicates, which have been more thoroughly studied and