augite信息详情
n.[矿物]辉石；普通辉石
dugite───n.拟眼镜蛇属
alunite───n.明矾石
augitic───adj.辉石的
auguste───n.笨拙型马戏团小丑
azurite───n.蓝铜矿
bauxite───n.矾土，[矿物]铁铝氧石；[矿物]铝土矿
dugites───杜吉特
turgite───n.[矿物]水赤铁矿
Gunite───n.[建]压力喷浆；喷射的水泥砂浆
Pyroxene is exclusively diopside augite, with a composition relatively close to the diopside - hedenbergite join.───辉石是透辉石质普通辉石，其成分相对近于透辉石- -镁铁辉石。
The groundmass has the same mineral components as phenocryst, and is composed of plagioclase, augite and olivine.───分析显示，基质矿物组成与斑晶矿物组成相同，均是由斜长石、辉石和橄榄石组成；
Pyroxene is exclusively diopsidic augite, with a composition relatively close to the diopside-hedenbergite join.───所有辉石是透辉石质普通辉石，其成分相对近于透辉石--镁铁辉石。
Main crystallization phase of glass ceramic was hedenbergite, and the minor crystallization phases were augite and hypersthene.───矿渣微晶玻璃的主析晶相为钙铁辉石，次晶相为普通辉石和紫苏辉石；
The rock stack is made up of various sized black or dark grey olivine, augite basalt, amphibole and andesite.───此岩系由黑色或暗灰色橄榄石、普通辉石玄武岩、角闪石安山岩等大小石块构成。
Discovery of orderly orbicular structures in megacrystalline augite───辉石巨晶中有序排列球体构造的发现
The groundmass has the same mineral components as phenocryst, and is composed of plagioclase, augite and olivine.
Chaoshan gold deposit is located at the Shizishan ore-field in Tongling, Anhui Province and the host rock is the Baimangshan augite diorite.
Latites contain plagioclase feldspar ( andesine or oligoclase) as large, single crystals (phenocrysts) in a fine-grained matrix of orthoclase feldspar and augite.
The effect of gangue minerals (serpentine, olivine and augite) containing magnesium onpentlandite flotation has been studied in this paper.
Pyroxene is exclusively diopsidic augite, with a composition relatively colse to the diopside - hedenbergite join.
The study of petrology, mineralogy and geochemistry suggests that augite latite and augite monzonite are cognate, belonging to the upper and root parts of the volcanic dome respectively.
Thyon volcanic rocks are classified as alkali basalts, with pyroxene megacrysts, and deep-seated mantle xenoliths such as augite and peridotite have been observed in some basaltic layers.
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Augite monzonite crystallized at high-temperature and over-hypabyssal conditions. The water-deficient, highly viscous magma was favourable to the formation of the volcanic dome.