「pyroxene」の共起表現(1語右で並び替え)

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共起表現

「pyroxene」の共起表現一覧(1語右で並び替え)

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rock-forming mafic minerals include olivine,	pyroxene, amphibole, and biotite.
dark porphyritic basanite which has abundant	pyroxene and olivine phenocrysts.
Biotite, hornblende,	pyroxene and scarce olivine or quartz are common acces
form intrusion via in-situ crystallisation of	pyroxene and plagioclase, or as part of a layered intr
It is composed mostly of	pyroxene and is thought to have undergone preterrestri
ite, monazite, nepheline, pyrite, pyrochlore,	pyroxene and quartz.
-spinel basalt with abundant large pale green	pyroxene and minor yellow-brown olivine phenocrysts.".
erovskite, aluminous spinel, hibonite, calcic	pyroxene, and forsterite-rich olivine.
hich is composed of the minerals plagioclase,	pyroxene, and olivine.
nepheline syenite with aegerine-augite as the	pyroxene, and with the addition of plagioclase (andesi
ferromagnesian silicates, such as amphibole,	pyroxene, and biotite.
ess pointed end) that is noticeably richer in	pyroxene, and has a generally basaltic composition.
covite, nepheline, olivine, perthite, pyrite,	pyroxene and pyrrhotite.
1: olivine crystallizes; 2: olivine and	pyroxene crystallize; 3: pyroxene and plagioclase crys
e conditions of the Earth's lower mantle, the	pyroxene enstatite, MgSiO3, transforms into a denser p
Since it is a member of the	pyroxene family, there is a great deal of interest in
with a strong, broad 1 micrometre olivine and	pyroxene feature, and a spectral slope that indiciates
When the	pyroxene fibers are coarser, they may appear to radiat
or minerals such as enstatite (magnesium-rich	pyroxene), forsterite (magnesium-rich olivine) and fel
CaFeSi2O6, is the iron rich end member of the	pyroxene group having a monoclinic crystal system.
sed of any of the following; titanium augite (	pyroxene), hornblende and biotite.
rmine whether forsterite olivine or enstatite	pyroxene is precipitated, but the water content and pr
Diopside is a monoclinic	pyroxene mineral with composition MgCaSi2O6.
es the "lustre-mottled" structure arises from	pyroxene or hornblende enveloping olivine in the same
ed intrusions in either the olivine-chromite,	pyroxene, or plagioclase-rich layers.
metamorphic rocks of the continents contains	pyroxene, plagioclase feldspar and accessory garnet, o
ns in the abundance of crystallizing olivine,	pyroxene, plagioclase and magnetite.
e only area in the basin not dominated by the	pyroxene rocks typical of lunar lowlands.
rimarily of the silicate minerals olivine and	pyroxene, surrounded by feldspathic material that may
ues for silicate minerals such as olivine and	pyroxene, which make up many of the rocky objects in t
nce of strong absorption lines in olivine and	pyroxene with little or no metals.
ocean proceeded, minerals such as olivine and	pyroxene would have precipitated and sunk to form the
ns in the common mantle minerals, olivine and	pyroxene, would occur within the pressure regime of th

共起表現

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「pyroxene」の共起表現一覧(1語右で並び替え)