「Magnetite」の共起表現(1語右で並び替え)

「Magnetite」の共起表現一覧(1語右で並び替え)

Magnetite

1語右で並び替え

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te, zircon, monazite, uraninite, aeschynite, magnetite, albite, topaz, beryl, garnet, muscovite and
The main minerals were magnetite and chondrodite.
s to somewhat intermediate character between MAGnetite and HEMatite.
with: sibirskite, calcite, dolomite, garnet, magnetite and pyroxene.
c igneous rocks contain grains of intergrown magnetite and ilmenite, formed by the oxidation of ulv
nt town are so named due to the existence of magnetite and the terrain being a cove, a basin-shaped
ch as the iron-bearing spinels hercynite and magnetite, and also rutile (titania).
s including chromium, vanadium, titaniferous magnetite and platinum group metals.
s of other heavy minerals, garnet, ilmenite, magnetite and pyroxene.
e remainder of the void space is filled with magnetite ballast with the entire structure weighing i
perating in the area are also planning major magnetite BIF based iron ore mines
ls that anandite is associated with include: magnetite, chalcopyrite, pyrite, pyrrhotite and baryte
For example, microscopic magnetite crystals in the Martian meteorite ALH84001 w
As such, cuprospinel is essentially magnetite doped with copper and this enhances magnetit
e-pyrite alteration, often with hematite and magnetite facies
It comprises mainly magnetite, Fe3O4, and as such is attracted to magnets.
ngs to the spinel group of minerals, as does magnetite, Fe3O4.
Greigite, Fe3S4, analog to magnetite, Fe3O4;
Magnetite formations near the summit are known to disr
It occurs in association with magnetite, forsterite, clinohumite and the borates von
It occurs in association with magnetite, garnet, fluorite, albite, cassiterite, pyri
own to exhibit framboidal structures include magnetite, hematite, and greigite.
Trace mineralogy may include magnetite, ilmenite and accessory olivine (<5%).
few percent, of iron-titanium oxides such as magnetite, ilmenite, and ulvospinel.
It is common in titaniferous magnetite iron ore deposits.
lts are important to plate tectonics because magnetite is an important recorder of rock magnetism.
The formula for magnetite is more accurately written as FeO.Fe2O3 than
Ordinary magnetite is attracted to a magnetic field like iron a
wet separators, a very dense medium (such as magnetite) is introduced into an agitated mixture of c
The interest of cuprospinel arises in that magnetite is a widely used catalyst for many industria
e, the ore is ground into a fine powder, the magnetite is separated from the waste rock by strong m
rs track the creature and her offspring to a magnetite mine.
Magnetite mining operations would require the construc
nites, amphibole, apatite, biotite, calcite, magnetite, monazite, nepheline, pyrite, pyrochlore, py
ite, fluorite, garnet, hematite, kaersutite, magnetite, muscovite, nepheline, olivine, perthite, py
Only a small amount of the magnetite on Earth is found magnetized as lodestone.
Not to be confused with Magnesite, Magnetite, or Magnemite.
Sashikomi nugui is usually composed of magnetite or tsushima and other compounds depending up
Substantial quantities of magnetite ore are also understood to exist on their ho
ements at Koolanooka South, with reserves of magnetite ore.
erials usually consist primarily of a black, magnetite sand with whatever gemstones or metal dust t
are hornblende-, chlorite-, haematite-, and magnetite- schists, felspathic schists: quartzites and
agnesium iron oxide mineral, a member of the magnetite series of spinels.
ned due to weathering of these ludwigite and magnetite skarns.
It occurs in association with magnetite, sphalerite, chalcopyrite, skutterudite, all
It has the same structure as magnetite, that is, it is spinel ferrite and is also f
ruit demons and use them to battle with, but Magnetite, the game's money, depletes with each use.
formed from other iron oxides, hematite and magnetite; the carbonate siderite and iron rich silica
ccurs associated with ilmenite, titaniferous magnetite, titanite, anatase, perovskite, baddeleyite,
dicating solid solution between ilmenite and magnetite, until the oxidation reaction and resultant
cessory minerals include apatite, zircon and magnetite, with rare biotite, hornblende or pyroxene.
nt research has found that only a variety of magnetite with a particular crystalline structure, a m
It has been shown that doping magnetite with other elements gives it different chemi
partial solid solution between trevorite and magnetite, with many magnetites from ultramafic rocks