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研究了全新世和更新世100多个向海块体运动沉积,其运动过程可分为3大类型(滑动/滑塌,塑性流和浊流),已识别出其中13种主要类型。这3大类型的区别主要在于运动形式、构型和破裂面形状。滑动沉积物的形态通常与运动过程有关,而塑性流和浊流运动过程的信息主要由沉积记录提供。基于这些特征,拟定了一个以动力学为分类体系的静态分类方案,主要强调向海事件从发生到沉积的过程中沉积物的形态变化。
The Holocene and Pleistocene more than 100 sea-to-sea block sediments were studied. Their movement processes can be divided into three major types (slip / slump, plastic flow and turbid flow), of which 13 main types have been identified. The three major types of differences are mainly in the form of movement, configuration and rupture surface shape. The morphology of the sliding sediments is usually related to the movement process, while the information of the plastic flow and turbidity flow movement is mainly provided by sedimentary records. Based on these characteristics, a static classification scheme based on dynamics is formulated, which mainly emphasizes the change of sediments in the process of sea events from occurrence to deposition.