Passive margins are characterized by rifted, rotated fault blocks of thick sediment, such as the present-day Gulf of Mexico and Atlantic margins of North America.
被动边缘以有厚沉积物的、有裂谷作用的旋转断块为特征。如现今的墨西哥湾和北美的大西洋边缘。
These ore deposits displaying belteddistribution mainly occurred in rift and passive continental margins, related to the syndepositional fractures.
在空间上有成带分布特点，主要分布在裂谷带和被动大陆边缘，与同生断裂密切相关。
Detachment models can also applied to the formation of passive continental margins.
伸展区剥离断层模式同样适用于被动大陆边缘的形成和演化。
Detachment models can also applied to the formation of passive continental margins.
伸展区剥离断层模式同样适用于被动大陆边缘的形成和演化。
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