登巴东剖面则代表了洋岛火山岩发育的晚期阶段，顶部有酸性熔岩的夹层，火山岩之上连续沉积有灰岩和砂岩。
The East Dengba section is a record of the late stage of oceanic island development, with interbeds of acid lavas at the top, overlain by continuous deposits of limestone and sandstone.
坡折带的发育演化具有明显的阶段性和继承性：早期为断裂坡折带，晚期为挠曲坡折带。
The development and evolution of the slope-breaks are episodic and successive: in early period, it is faulted slope-break; in later period, it is flexural slope-break.
鸭嘴龙超科的骨骼化石和分散的恐龙蛋共存于同一层位，大部分的骨骼化石属于未离巢晚期和幼年早期的个体发育阶段。
The hadrosauroid remains occur with scattered dinosaur eggs at the same horizon. The majority of the bones may come from the late nestling and early juvenile stages.
鸭嘴龙超科的骨骼化石和分散的恐龙蛋共存于同一层位，大部分的骨骼化石属于未离巢晚期和幼年早期的个体发育阶段。
The hadrosauroid remains occur with scattered dinosaur eggs at the same horizon. The majority of the bones may come from the late nestling and early juvenile stages.
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