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中间圈包括岩流圈以下地幔的其余部分。The mesosphere comprises the rest of the mantle below the asthenosphere.

该阶段的碱性玄武岩浆可能来源于软流圈。The alkalic basaltic magma of this stage may be derived from asthenosphere.

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在均衡校正中有时将其作为软流层的顶部。Involved in isostatic correction sometimes taken as the top of the asthenosphere.

冲绳海槽仍是一个软流圈在汇聚的弧后盆地。The Okinawa Trough is a back arc basin still driven by the converging asthenosphere.

岩石圈和软流圈的差异运动导致了天山新生代构造变形。The differential movement of lithosphere and asthenosphere causes the Neozoic deformation of Tianshan.

板块和软流圈之间不同的相对运动机制是形成不同类型造山作用的主要原因。The orogenic types were controlled by the relative motion mechanism between lithosphere and asthenosphere.

软流层隆升对大型含油气区形成具有决定性意义。It presents a decided signification that the asthenosphere rised to the forming of big petroliferous regions.

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软流圈上涌高度、莫霍面或地幔羽的位置是地幔对流的具体的表现。The rise of the asthenosphere , the position of Moho and mantle plume are the indication of the mantle convection.

板缘造山主要表现为岩石圈和软流圈以基本相同的运动趋势的相对运动。Maginal orogeny was formed on this condition with same relative motion trend between lithosphere and asthenosphere.

石油的热动力平衡计算也证明石油形成于地幔软流层部位。The petroleum thermodynamic equilibrium calculation demonstrates that oils can be originated in mantle's asthenosphere.

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

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。Both depleted and fertile mantle domains are likely to be mechanically juxtaposed in the asthenosphere in a state of 'plum pudding'.

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青藏高原内部软流圈具有低密度特征，低密度软流圈产生向上的浮力是青藏高原重要的隆升机制之一。The asthenosphere is of low density in Tibet, and the upward buoyancy it caused seems to be one of the uplift mechanisms in Tibet plateau.

根据前人的研究，软流圈的上隆可能受控于东西向拉张作用引发的岩石圈减薄作用。According to the previous studies, the uplifting of the asthenosphere could be correlated with lithosphere thinning resulted from an E-W extension.

板块分离时，岩石圈或地壳象盖子般移到一旁，液态软流层中的熔岩渗溢而出。As the plates spread apart, the lithosphere, or crust, is moved aside like a lid, allowing molten rock from the liquid asthenosphere to seep through.

结果显示，在海沟及其洋侧冷的软流层发生了大规模的沉降，而弧后热的软流层则强烈抬升。The conversion result shows that the cold asthenosphere sinks in large scale along trenches and ocean-sides and hot asthenosphere rises greatly along the arc-back area.

我们初步认为，该区深部岩石圈MORB-OIB地幔可能是软流圈置换古岩石圈地幔而增生形成的。It is tentatively suggested that the lower lithosphere MORB-OIB mantle is recently accreted since the paleo-lithosphere mantle was replaced by the abnormal asthenosphere.

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中生代壳幔相互作用明显，克拉通稳定时期及新生代时期层圈之间相互作用的活跃带位于岩石圈与软流圈之间。In Mesozoic, the most important interaction occurred between the crust and the mantle, whereas in the older and Cenozoic it did between the lithosphere and the asthenosphere.

地幔柱产生大面积软流圈上涌，沿深断裂形成岩浆房，导致大规模溢流玄武岩裂隙式喷发。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.

断裂带在晚白垩世-早第三纪的伸展活动中，软流圈进行了强烈的上隆，岩石圈出现了显著的细颈化，属于纯剪切伸展模式。During extensional activities of Late Cretaceo us to Eogene, intense upwelling of asthenosphere happened under the fault zone, leading to lithospheric necking in pure shear mode1.