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复数形式
asthenospheres
1
软流圈, 地壳下半流体的岩石层
a layer of semi-fluid rock beneath the Earth's crust that allows tectonic plates to move
- The asthenosphere's flow allows for the movement of tectonic plates, contributing to Earth's dynamic crustal activity.
软流圈的流动使得构造板块能够移动，从而促进地球动态地壳活动。
- Seismic waves passing through the asthenosphere reveal its semi-fluid nature and lower resistance to deformation.
穿过软流圈的地震波揭示了其半流体的性质和较低的变形阻力。
- It plays a role in the formation of mid-ocean ridges, where magma rises from the asthenosphere, creating new oceanic crust.
它在洋中脊的形成中发挥作用，岩浆从软流圈上升，形成新的海洋地壳。
- The ductile properties of the asthenosphere allow it to absorb stress and strain, reducing the likelihood of brittle failure.
软流圈的韧性特性使其能够吸收应力和应变，降低脆性破坏的可能性。
- The movement of magma from the asthenosphere to the Earth's surface leads to volcanic activity in regions like the Pacific Ring of Fire.
岩浆从软流圈向地球表面的移动导致了环太平洋火山带等地区的火山活动。