论文部分内容阅读
构成陆棚与弧后盆地分界之贵州中三叠世礁型大陆边缘,在其礁缘斜坡上发育了碳酸盐岩碎屑流,该碎屑流为滑塌沉积,而非滑坡沉积。滑塌的原因与礁的快速堆积有关。
Carbonate debris flow is developed on the margins of the reef margin of the Middle Triassic reef continental margin forming the boundary between the shelf and the backarc basin. This debris flow is a slump deposit rather than a landslide deposit. The reason for the collapse is related to the rapid accumulation of reefs.