「SILICATES」の共起表現(1語右で並び替え)

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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

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