peridotite
美 [?per?'do?ta?t] 
英 [?per?'d??ta?t]
- n.【礦】橄欖巖
- 網(wǎng)絡(luò)橄欖石；橄巖；姍勬
英漢解釋
英英解釋
例句
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.
科研小組已經(jīng)證明，阿曼的橄欖巖每年能吸收數(shù)以萬噸的二氧化碳，這大大地超過了人們的想象。
The osmium isotopic compositions and model age of mantle peridotite xenoliths from Jiangsu-Anhui area and their geological significance.
蘇皖地區(qū)幔源橄欖巖捕虜體的鋨同位素組成、模式年齡及其意義。
This may be up to 50km thick and comprises ultrabasic peridotite.
其厚度可達(dá)50公里并由超基性的橄欖巖所組成。
Like basalt, peridotite chemically reacts with carbon dioxide-saturated water to quickly form minerals, some of which contain carbon.
橄欖巖像玄武巖一樣和二氧化碳飽和溶液發(fā)生化學(xué)反應(yīng)后能迅速生成礦物質(zhì)，其中一些含有碳。
of compound rock-body. They belong to mafic, ultramafic rocks which type are gabbro, pyroxenite and peridotite.
與銅鎳礦成礦有關(guān)的巖體具有復(fù)合雜巖體特征，多屬輝長巖—輝石巖—橄欖巖型鎂鐵—超鎂鐵質(zhì)巖。
Ultrabasic rocks have a silica content less than 45%. Peridotite is the typical intrusive rock which consists of olivine and pyroxene.
超基性巖的SiO2含量小于45%，它的侵入巖叫做橄欖巖，主要由橄欖石、輝石等礦物組成。
The Karamaili ophiolite complex in East Junggar of Xinjiang province is composed of metamorphic peridotite, gabbro, diabase and basic lava.
卡拉麥里蛇綠混雜巖的巖石組合為變質(zhì)橄欖巖、輝長巖、輝綠巖和基性熔巖等。
Cr ore deposits are genetical divided into 2 types ie. magmatic type and relic and stagnated type of metamorphosed mantle peridotite.
鉻鐵礦床成因可分為兩大類：巖漿鉻鐵礦床和地幔變質(zhì)橄欖巖殘、滯留鉻鐵礦床。
Peridotite occurs in sizable and accessible quantities on every continent except Antarctica, according to Kelemen.
據(jù)科勒曼說，在除了南極洲以外的所有大陸都能相當(dāng)容易地找到大量的橄欖巖。
The magnesite originated from the peridotite by weathering.
菱鎂礦是由橄欖巖風(fēng)化形成的。
When carbon dioxide comes in contact with the rock, peridotite, the gas is converted into solid minerals such as calcite.
當(dāng)二氧化碳與橄欖巖接觸時，氣體會被轉(zhuǎn)化成固態(tài)類似方解石的物質(zhì)。
Peridotite-melt interaction: an important mechanism for the compositional transformation of lithospheric mantle
橄欖巖-熔體的相互作用：巖石圈地幔組成轉(zhuǎn)變的重要方式
research on quantitative relation between multi - angle polarized reflectance and bi - directional reflectance of peridotite
橄欖巖的多角度偏振與二向反射定量關(guān)系研究
Geochemistry of super-magnesium peridotite in the Houxianyu boron deposit, Yingkou, Liaoning, and its constraints on the source region
遼寧營口后仙峪超鎂橄欖巖的地質(zhì)地球化學(xué)特征及其對源區(qū)的約束
the solubility and existing state of water in crystals of peridotite at high temperature and pressure;
高溫高壓下水在橄欖石晶體中的溶解度和賦存狀態(tài)；
Two types of peridotite in continental orogenic belts-a case study from the North Qaidam UHP metamorphic belt
大陸碰撞造山帶的兩類橄欖巖——以柴北緣超高壓變質(zhì)帶為例
Oxygen isotope and trace element compositions of peridotite xenoliths from Panshishan volcano, SE China
江蘇盤石山玄武巖中橄欖巖包體的氧同位素和微量元素地球化學(xué)
Ophiolite-type mantle peridotite from Shaliuhe, North Qaidam UHPM belt, NW China and its tectonic implications
柴北緣超高壓變質(zhì)帶沙柳河蛇綠巖型地幔橄欖巖及其意義
Ore-control role of ultra-magnesium peridotite in Houxianyu boron ore district, Yingkou, Liaoning Province
遼寧營口后仙峪硼礦區(qū)超鎂橄欖巖的控礦作用
On the naming of peridotite facies of the Hongqiling No. 1 Rock body ore-bearing of Jilin Province
關(guān)于吉林紅旗嶺1號含礦巖體橄欖巖相的定名問題
