1) passive continental margin basins
被动陆缘盆地
2) passive margin basin
被动大陆边缘盆地
1.
The Mauritania Coast Basin represents a classical passive margin basin created in response to the opening and drift of the Atlantic Ocean,which began in the Late Permian/Early Triassic times.
毛里塔尼亚海岸盆地位于非洲西部大西洋东岸,是典型的中新生代被动大陆边缘盆地。
3) residual basin of passive continental margin
残留被动大陆边缘盆地
1.
One type of basin known as "residual basin of passive continental margin" has been overlooked in all basin classifications.
各种盆地分类中人们忽略了一种盆地类型,即“残留被动大陆边缘盆地”。
4) passive margin of back-arc basin
弧后盆地被动陆缘
6) passive continental margin
被动陆缘
1.
They were continental rift and passive continental margin basins formed as a result of the break-up of Gondwana and the spreading of Atlantic Ocean.
西非海岸盆地群的形成和发育,与中生代以来大西洋裂开和后期的持续扩张作用有关,是冈瓦纳大陆解体和大西洋扩张形成的大陆裂谷和被动陆缘盆地。
补充资料：陆缘冰
又称“冰架”、“冰棚”或“冰障”。大陆冰川向海洋伸展，其漂在海上的冰体。陆缘冰断裂后入海，即形成冰山。最著名的是南极大陆外围的罗斯冰架(陆缘冰)。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条