In earlier stage, blueschists had staled at the lower crust level of accretionary wedge for about 00Ma, only slight uplift having happened, at a rate of about 0.0 - 0.mm /a, caused by buoyant forces.
In earlier stage, blueschists had staled at the lower crust level of accretionary wedge for about 00Ma, only slight uplift having happened, at a rate of about 0.0 - 0.mm /a, caused by buoyant forces.
早期阶段,蓝片岩在增生楔下部的下地壳深处滞留了约00Ma,仅因浮力作用发生轻微抬升,速率约0.0—0.mm/a。