Most of the rocks might be originally fragments of oceanic rocks introduced during plate subduction.
这些岩石大部分可能为板块俯冲过程中带入的大洋岩石残片。
Therefore the formation of these rocks is related to plate subduction.
因而这些岩石的形成与板块俯冲有关。
The eruption of Mount St. Helens in 1980 was the direct result of plate subduction.
圣海伦火山在 1980 年的喷发是板块沉降的直接结果。
Qiaohuote copper deposit, located at suture zone of Nalati plate, is medium-sized ore related to plate subduction.
乔霍特铜矿床位于那拉提板块缝合带上，是与板块俯冲作用有关的中型矿床。
Forming of the force of center uplifting and lateral compressing depends on the size of dip Angle of plate subduction.
中央隆升力和侧向挤压力的形成取决于板块俯冲倾角的大小。
In Cenozoic typical back-arc rift basins are formed in ne China where is the back-arc area of Pacific plate subduction zone.
新生代，东北地区作为太平洋板块俯冲带的弧后地区，形成了典型的弧后裂谷盆地。
It is one of the evidences of the earliest plate subduction at the south margin of the ancient continental plate of North China.
这是华北古大陆板块南部最早的板块俯冲活动的证据之一。
The tectonism of North China platform had the multistage plate subduction and collision which form a favourable condition for gold mineralization.
华北地台区构造作用具有多期次板块俯冲和碰撞，是金矿形成的有利条件。
The enrichment of the HFS elements such as Nb, Ta, Zr, Hf suggests that the forming environment of Zedang ophiolite is not related to plate subduction.
Hf等高场强元素较为富集，反映出泽当蛇绿岩的形成并未受到俯冲作用的影响。
In this paper, we mainly use plate subduction model to calculate and simulate some major subduction boundaries all over the world, and discuss the problem of the dip Angle.
文中主要通过平板俯冲模型来计算模拟全球范围内一些大的俯冲边界，并对俯冲角等问题作了一些讨论。
Following the Triassic collision, with Pacific plate subduction and continuous accumulation towards Eurasian plate in the Jurassic-Cenozoic, the huge accretionary complex belt was eventually formed.
侏罗纪—新生代在三叠纪碰撞基础上，太平洋板块向欧亚大陆连续俯冲和加积，进而形成由三叠纪—新生代杂岩组成的欧亚大陆东部地区的巨大加积杂岩带。
Following the Triassic collision, with Pacific plate subduction and continuous accumulation towards Eurasian plate in the Jurassic-Cenozoic, the huge accretionary complex belt was eventually formed.
侏罗纪—新生代在三叠纪碰撞基础上，太平洋板块向欧亚大陆连续俯冲和加积，进而形成由三叠纪—新生代杂岩组成的欧亚大陆东部地区的巨大加积杂岩带。
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