拆离引起拉伸的固有不对称性导致了共扼型的且具明显差异的被动陆缘。上板块陆缘组成深部拆离之上的地壳。下板块陆缘组成拆离底板，已被断开的上板块残余覆盖。这些陆缘有独特的结构样式、构造类型、隆起－沉降轨迹和热历史。被动陆缘上构造类型的多样性通过同时作用于与水平韧性剪切带和剪切带之下热岩石圈韧性拉伸作用有关的拆离断层上的五个模式来预测。这些模式对被动陆缘上不可思议的构造和地貌特征──陆缘高地、外侧高地、未受构造作用的裂谷同期凹陷盆地及位于高地的断裂盆地作了解释。地壳均衡隆起－沉降历史的数字模型表明隆起－沉降特性的各种型式可用拆离几何学的变化和岩石圈拉伸作用的大小变化来解释。如果热软流圈异常隆起，就可预测有大量岩浆垫托作用。这种地幔派生的熔体的就位可引起有效的辅助隆起。上面板块边缘经受的热诱导隆起由于岩浆垫托作用而具持久性。这种隆起可能是邻接腹地中被动陆缘山脉形成的原因。陆缘高地的上升，或非常缓慢的沉降贯穿了整个拉伸历史，即使裂谷期后沉降到中等水平的深度。岩石圈在中地壳拆离之下扩张，但上板块很少拉伸。大西洋陆缘的沉降格式需要在渐进拉伸的拆离面下岩石圈上叠加一个拉张的板块。描述的共扼陆缘取材于塔斯曼海、大西洋和大南洋，? The inherent asymmetry in tension caused by detaching results in a conjugate and clearly differentiated passive margin. On the plate composed of the continental margin deep detachment of the crust. Under the plate composed of the continental floor detachment of the floor, has been disconnected on the plate residual coverage. These continental margins have unique structural patterns, tectonic types, uplift-subsidence trajectories and thermal history. The diversity of tectonic types on the passive margins is predicted by five modes simultaneously acting on the detachment faults associated with the ductile stretching of the hot-lithosphere under horizontal ductile shear zones and shear zones. These models explain the incredible tectonic and geomorphological features of the passive margin - the marginal highlands, the outer highlands, unconformity rift syncocene basins, and the fault basins located in the highlands. The crustal crustal uplift-sedimentation history numerical model shows that the various types of uplift-subsidence characteristics can be explained by the change in detach geometry and the magnitude of lithospheric stretch. If the thermal asthenospheric anomaly uplift, you can predict a large number of magmatic mat role. The mantle-derived melt in place causes effective secondary bumps. The thermally induced ridges experienced by the edges of the upper plate persisted due to the magmatic underlayment. This uplift may be due to the formation of the passive continental rim in the hinterland. The rise in marginal highlands, or very slow subsidence, runs through the entire stretch history, even after settlement to a moderate depth after the rifting period. The lithosphere expanded under the disintegration of the middle crust, but the upper plate rarely stretched. The subsidence format of the Atlantic margin requires the superimposition of a tensioned plate on the lithosphere below the progressively stretched detachment. The described conjugate margins are based on the Tasman Sea, the Atlantic and the Great South Seas.