根据从珊瑚海和日本海海底扇回收的深海钻井计划岩芯的序粒旋回推测保存下来的浊流沉积事件的频率。这种沉积事件分别与巴布亚岛欧文-斯坦利山脉和日本飞(马单)山脉的构造抬升鼎盛期有关。保存下来的浊流沉积事件频率的增高和降低分别与构造抬升速率的速率的增快和减慢趋势有关。因此,沉积盆地中单独保存下来的浊流沉积事件的频率为测定毗邻源区造构升抬的相对速率提供了一个独立的论据。 The frequency of turbidity-flow sedimentation events preserved was estimated from the sequence-based gyration of deep-sea drilling program cores recovered from coral and sea submarine fans of the Japan Sea. This depositional event was related to the peak tectonic uplift of the Owen-Stanley and Papua New Guinea Ranges in Papua. The increase and decrease of the frequency of the preserved turbidity flow sedimentation events are respectively related to the trend of increasing and slowing the rate of tectonic uplift. Therefore, the frequency of turbidite sedimentary events separately deposited in sedimentary basins provides an independent argument for determining the relative rates of structural lift in adjacent source regions.