asthenosphere信息详情
n.[地质]软流圈；岩流圈
myasthenia gravis───[内科]重症肌无力；假麻痹性重症肌无力，重症肌无力
asthenic───n.身体虚弱的人；体型瘦长之人；adj.衰弱的；瘦长的
asthenic disarders───衰弱症
asthenia of renal yin───[医]肾阴虚，肾水不足，真阴不足
Megasthenes───巨实
asthenic gout───虚痛风
asthenic voice───无力的声音
amasthenic───无感觉的
asthenia───n.[临床]无力；[医]衰弱
asthenopia───n.[眼科]视力疲劳；[眼科]眼疲劳
The alkalic basaltic magma of this stage may be derived from asthenosphere.───该阶段的碱性玄武岩浆可能来源于软流圈。
The mesosphere comprises the rest of the mantle below the asthenosphere.───中间圈包括岩流圈以下地幔的其余部分。
The asthenosphere corresponds approximately to the low - velocity zone.───软流圈，大体上相当于低速带。
Both depleted and fertile mantle domains are likely to be mechanically juxtaposed in the asthenosphere in a state of 'plum pudding'.───亏损和饱满的地幔域在软流圈中可能被机械地堆积在一起。
It presents a decided signification that the asthenosphere rised to the forming of big petroliferous regions.───软流层隆升对大型含油气区形成具有决定性意义。
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公里的上地幔顶部被称为软流层
The decompression melting fluid system of asthenosphere provides the driving force for magma emplacement and metallogenic material.───软流圈减压熔融流体系统提供了岩浆侵位动力和成矿物质来源。
The asthenosphere formed in a large scale after Mesozoic.───中生代以后，软流层大规模发育。
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.