An interaction of lithospheric plates that can result in the formation of mountain belts and subduction zones.
一种可导致形成造山带和俯冲带的岩石圈板块间的相互作用。
Such alteration occurs as rocks respond to changes in temperatures, pressures and fluids, commonly along the edges of colliding lithospheric plates.
这样的蚀变作用是岩石对温度、压力和流体的变化的反响,通常沿着碰撞的岩石圈板块的边沿发生。
Such alteration occurs as rocks respond to changes in temperatures, pressures and fluids, commonly along the edges of colliding lithospheric plates.
这样的蚀变作用是岩石对温度、压力和流体的变化的反响,通常沿着碰撞的岩石圈板块的边沿发生。
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