大陆隆
dà lù lónɡ
- continental rise;continental apron
大陆隆
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构造事件的沉积响应&建立青藏高原大陆碰撞、隆升过程时空坐标的设想和方法
Sedimentary response to tectonic events : Reconstructed spatio-temporal scale of the Indo-Asian continental collision and Qinghai-Xizang Plateau uplift
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青藏高原第四纪大陆冰盖对高原隆升的影响
The effects of the Quaternary Continental glacial sheet in Qinghai-Xizang Plateau upon the uplift of the plateau
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而在本组沉积晚期,水体开始变浅,大致为大陆斜坡-陆隆半深海浊流沉积环境。
During the late period of sedimentation , however , the water depth became shallower as the environment of turbidity current in continental slope rising .