peridotite [,peri'dəutait]
- peridotite的基本解释
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n.
橄榄岩
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A rock formation in South Africa containing peridotite, in which diamonds are formed.
金伯利岩南非的一种包含橄榄岩的岩层,岩层中形成了钻石
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Peridotite can also be found at the surface in other parts of the world, including some Pacific islands, along the coasts of Greece and Croatia, and in smaller deposits in America.
橄榄岩也可以在地表的其他地方找到,包括一些太平洋岛屿,希腊和克罗地亚的沿岸,和美国的一些较小的矿场上。
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The team has shown that the Omani peridotite absorbs tens of thousands of tonnes of carbon dioxide a year, far more than anyone had thought.
该小组已经证明,阿曼的橄榄岩每年能吸收数以万吨的二氧化碳,这大大地超过了人们的想象。
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Research on quantitative relation between multi-angle polarized reflectance and bi-directional reflectance of peridotite .
橄榄岩的多角度偏振与二向反射定量关系研究。
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The rock is peridotite, which is one of t he main rocks in the upper mantle, an area that provides a girth below the Earth's crust.
这种岩石是橄榄岩,是上地幔的主要组成成分,地幔是地壳以下围绕地球一周的区域。
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- 更多网络解释与peridotite相关的网络解释 [注:此内容来源于网络,仅供参考]
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peridotite:橄榄岩
细小至肉眼不能辨识者为流纹岩(Rhyolite);晶体粗大之中性火成岩为闪长岩(Diorite)细小者为安山岩(Andesite);晶体粗大之基性火成岩为辉长(Gabbro),细小者为玄武岩(Basalt);晶体粗大之超基性火成岩为橄榄岩(Peridotite),此种火成岩无晶体
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peridotite:橄岩
Percussion boring 式孔 | Peridotite 橄岩 | Permafrost 永土
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peridotite:橄榄绿
percolation - 渗流,渗滤,渗透 | Peridotite - 橄榄绿 | permeability - 渗透性,导磁率,透射率
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peridotite:橄榄石
granito 花岗石 | peridotite 橄榄石 | sienite 正长岩
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mica peridotite:云母橄榄岩
云母玢岩 mica-porphyrite | 云母橄欖岩 mica-peridotite | 云母海绿石质砂岩 gaize
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