?asthenosphere

asthenosphere 發(fā)音

英：[?s'θen?sf??]　　美：[?s'θin?,sf?r]

英：　　美：

asthenosphere 中文意思翻譯

asthenosphere 網(wǎng)絡(luò)釋義

n. [地質(zhì)] 軟流圈；巖流圈

asthenosphere 相似詞語(yǔ)短語(yǔ)

1、Megasthenes ─── 巨實(shí)

2、asthenia ─── n.[臨床]無(wú)力；[醫(yī)]衰弱

3、amasthenic ─── 無(wú)感覺(jué)的

4、myasthenia gravis ─── [內(nèi)科]重癥肌無(wú)力；假麻痹性重癥肌無(wú)力，重癥肌無(wú)力

5、asthenopia ─── n.[眼科]視力疲勞；[眼科]眼疲勞

6、asthenia of renal yin ─── [醫(yī)]腎陰虛，腎水不足，真陰不足

7、asthenic ─── n.身體虛弱的人；體型瘦長(zhǎng)之人；adj.衰弱的；瘦長(zhǎng)的

8、asthenic voice ─── 無(wú)力的聲音

9、asthenic gout ─── 虛痛風(fēng)

10、asthenic disarders ─── 衰弱癥

asthenosphere 常見(jiàn)例句（雙語(yǔ)使用場(chǎng)景）

1、The decompression melting fluid system of asthenosphere provides the driving force for magma emplacement and metallogenic material. ─── 軟流圈減壓熔融流體系統(tǒng)提供了巖漿侵位動(dòng)力和成礦物質(zhì)來(lái)源。

2、It presents a decided signification that the asthenosphere rised to the forming of big petroliferous regions. ─── 軟流層隆升對(duì)大型含油氣區(qū)形成具有決定性意義。

3、The alkalic basaltic magma of this stage may be derived from asthenosphere. ─── 該階段的堿性玄武巖漿可能來(lái)源于軟流圈。

4、The top layers of the upper mantle, 100 to 200 kilometers below surface, is called the asthenosphere. ─── 位于地表以下100到200公里的上地幔頂部被稱為軟流層

5、Both depleted and fertile mantle domains are likely to be mechanically juxtaposed in the asthenosphere in a state of 'plum pudding'. ─── 虧損和飽滿的地幔域在軟流圈中可能被機(jī)械地堆積在一起。

6、The asthenosphere corresponds approximately to the low - velocity zone. ─── 軟流圈，大體上相當(dāng)于低速帶。

7、The mesosphere comprises the rest of the mantle below the asthenosphere. ─── 中間圈包括巖流圈以下地幔的其余部分。

8、The asthenosphere formed in a large scale after Mesozoic. ─── 中生代以后，軟流層大規(guī)模發(fā)育。

英語(yǔ)使用場(chǎng)景

This would drag the underlying asthenosphere along and promote a compensatory upward movement within the mantle under mid-oceanic ridges.

The decompression melting fluid system of asthenosphere provides the driving force for magma emplacement and metallogenic material.

The asthenosphere corresponds approximately to the low - velocity zone.

The differential movement of lithosphere and asthenosphere causes the Neozoic deformation of Tianshan.

Forty-five miles beneath the surface, the layer known as the asthenosphere begins.

Asthenosphere uplift indicates the deep adjustment process during the interaction of plates, and also shows the adjusting process of gravitational equilibrium between upper layer of crust and mantle.

Mantle plumes induced asthenosphere upwelling and development of magma chambers along deep-sited faults, and thus resulted in fracture eruption of flood basalts on large scale.

The rise of the asthenosphere , the position of Moho and mantle plume are the indication of the mantle convection.

It presents a decided signification that the asthenosphere rised to the forming of big petroliferous regions.

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