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asthenosphere
英：【əsθenəsfɪə】美：【æsθinə,sfɪr】
英：
美：
常见释义：
n.
【地质】软流圈；岩流圈
n. 【地质】 软流圈；岩流圈
1、Megasthenes ─── 巨实
2、asthenia ─── n.【临床】无力；【医】衰弱
3、amasthenic ─── 无感觉的
4、myasthenia gravis ─── 【内科】重症肌无力；假麻痹性重症肌无力，重症肌无力
5、asthenopia ─── n.【眼科】视力疲劳；【眼科】眼疲劳
6、asthenia of renal yin ─── 【医】肾阴虚，肾水不足，真阴不足
7、asthenic ─── n.身体虚弱的人；体型瘦长之人；adj.衰弱的；瘦长的
8、asthenic voice ─── 无力的声音
9、asthenic gout ─── 虚痛风
10、asthenic disarders ─── 衰弱症
1、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。
2、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。
3、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。
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公里的上地幔顶部被称为软流层
5、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。
6、The
asthenosphere
corresponds approximately to the low - velocity zone. ─── 软流圈，大体上相当于低速带。
7、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。
8、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.