「Pyroxene」の共起表現一覧(1語右で並び替え)

Pyroxene

1語右で並び替え

該当件数:33件

  • 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