When a continental plate come to rest over a hot spot, the material rising from deeper layer creates a broad dome.
当大陆板块停留在一个热点上时,从深层升起的物质就会形成一个广阔的圆顶。
By measuring the slow rising and falling of the ground as the inexorable collision of the Nazca plate squeezed the coast, they could calculate how fast strain was actually building.
通过测量因纳斯卡板块挤压海岸发生碰撞造成的地面的缓慢上升与下降,他们能够估算压力的实际聚集速度。
Per the Zetas, this was due to the nature of the plate adjustments, which involved subduction, a lateral movement, rather than rising or falling land under water.
根据齐塔人的说法,这取决于板块调整的横向运动和俯冲特性,而不是海底发生了升降。
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