Calculations of the apatite-zircon mineral pair and results of thermal-simulation give the apparent uplift rate of each uplifting phase . The apparent uplift rate has generally increased since the late Cretaceous .
通过磷灰石-锆石矿物对计算以及热模拟的结果,获得了各隆升阶段的视隆升速率,发现自晚白垩世晚期以来,视隆升速率有逐渐增加的趋势。