「Pyroxene」の共起表現一覧(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 |
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