Profilo Traduttore: Jiacheng Zhu (woygwle)

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Chinese

Master of Applied Statistics | Multiple Translation Certificates | First Prize in Multiple Translation Competitions

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earth sciences

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Esempio di traduzione Earth Sciences

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Plate tectonics, mountain ranges, volcanoes, and earthquakes are geological phenomena that can be explained in terms of physical and chemical processes in the Earth's crust.	板块构造、山脉、火山和地震，是可以用地壳中的物理和化学过程来解释的地质现象。
Beneath the Earth's crust lies the mantle which is heated by the radioactive decay of heavy elements.	在地壳之下是地幔，它由重元素的放射性衰变加热。
The mantle is not quite solid and consists of magma which is in a state of semi-perpetual convection.	地幔并非完全是固态，而是由处于近乎持续对流状态的岩浆构成。
This convection process causes the lithospheric plates to move, albeit slowly.	这种对流过程导致岩石圈板块移动，尽管十分缓慢。
The resulting process is known as plate tectonics.	由此产生的过程被称为板块构造。
Plate tectonics might be thought of as the process by which the Earth is resurfaced.	板块构造可以被看作是地球表面被更新的过程。
As the result of seafloor spreading, new crust and lithosphere is created by the flow of magma from the mantle to the near surface, through fissures, where it cools and solidifies.	由于海底扩张，来自地幔的岩浆通过裂隙流向近地表，并在那里冷却并固结，从而形成新的地壳和岩石圈。
Through subduction, oceanic crust and lithosphere returns to the convecting mantle.	通过俯冲，海洋地壳和岩石圈回到正在对流的地幔中。
Areas of the crust where new crust is created are called divergent boundaries, those where it is brought back into the Earth are convergent boundaries and those where plates slide past each other, but no new lithospheric material is created or destroyed, are referred to as transform (or conservative) boundaries Earthquakes result from the movement of the lithospheric plates, and they often occur near convergent boundaries where parts of the crust are forced into the Earth as part of subduction.	在地壳中，生成新地壳的区域称为张裂边界，将其带回地球内部的区域称为汇聚边界，而那些板块彼此滑移、但不产生也不消灭新的岩石圈物质的区域则称为转换（或保守型）边界，地震源于岩石圈板块的运动，并且它们常发生在汇聚边界附近，在那里地壳的部分作为俯冲的一部分被压入地球内部。
Volcanoes result primarily from the melting of subducted crust material.	火山主要起因于被俯冲的地壳物质的熔融。
Crust material that is forced into the asthenosphere melts, and some portion of the melted material becomes light enough to rise to the surface—giving birth to volcanoes.	被压入软流圈的地壳物质发生熔融，其中一部分熔融物变得足够轻，能够上升到地表——从而孕育火山。

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