anorthosite [æ'nɔ:θəsait]
- anorthosite的基本解释
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斜长岩, 斜长石, 火成岩
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The anorthosite and similar rock types in the highlands and basalt lavas in the marea are the Moon's basic building blocks.
斜长岩和类似的岩石在高地典型,而玄武岩沉积在月球低地构成了月亮基本的建筑积木。
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Composed mainly of anorthosite and plagiogranite, the leucocratic rocks show distinct Eu positive anomaly.
浅色岩类的岩石类型包括斜长岩和斜长花岗岩,它们均呈岩块状包裹于蛇纹岩中。
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Although scientists had postulated this phase of lunar history based on the Apollo samples, the proof came from the Clementine and Lunar Prospector data, which indicated the global distribution and large abundance of anorthosite.
虽然科学家根据阿波罗太空船所采集的样本提出了关于月球这段历史的假说,但是证据却来自克莱门蒂号和月球探勘者号的观测,显示斜长岩丰富且分布全球。
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The RE E patterns of apatites in porphyrite iron deposits are in general similar to those of apatites in anorthosite, norite andjacupirangite . The apatites are enriched in light REE, with pronounced negative Eu anomaly.
结果表明产地和母岩不同的矿床中,它们的磷灰石稀土元素分布型式一致,以轻稀土富集和Eu负异常明显为特征,属陆相岩浆成因。
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Working from outside the basin in to the Mare Basalts, they find the surface composition changes from Feldspathic breccias (Feldspar is a rock that crystallizes from magma) to shocked Anorthosite (a type of feldspar that makes up the light areas of the moon), to unshocked crystalline anorthosite, to high Calcium pyroxene (a rock made of silicate minerals) and pyroclastic rocks in the center.
研究发现:从盆地外边到盆地内部的玄武岩海(盆地内部的熔岩形成的地质结构),月球表面的地质结构依次是:长石质的角砾岩(长石是火山熔岩结晶形成的岩石)、经过冲击的粒状火成岩(构成月球阳面的一种长石)、没有经过冲击的粒状火成岩结晶体、高钙辉石(一种由硅酸盐构成的岩石),最中心的位置是分裂状的火山岩石。
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anorthosite:斜长岩
斜长岩(anorthosite) 主要由斜长石组成,含量大于90%,斜长石一般为拉长石或中长石,暗色矿物为斜方辉石、单斜辉石、角闪石等,总和不足10%. 斜长岩具有半自形或它形粗粒结构.
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anorthosite:斜长石
anorthoclase 歪长石 | anorthosite 斜长石 | antarctic pole 南极
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anorthosite:火成岩
anorthitic 钙长石的 | anorthosite 火成岩 | anoscope 肛门窥器
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anorthosite:斜长岩;钙长岩
"斜长石","anorthose" | "斜长岩,钙长岩","anorthosite" | "斜长岩化作用","anorthositization"
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quartz anorthosite:石英斜长岩
quarto 四开;四开本;四开的 | quartz anorthosite 石英斜长岩 | quartz crystal oscillator gauge 石英晶体振荡压力计
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