The two tectonic systems are concrete manifestations of the active rifting and passive rifting mechanisms in the basin during the Cenozoic.
这两种构造系统是盆地区新生代时期主动裂陷和被动裂陷两种作用机制的具体表现。
The Okinawa Trough (OT) is the solitary active backarc basin in the world that is formed by extensional rifting in the continental marginal zone and is in the early stage of evolution.
冲绳海槽是当今世界上唯一的在大陆边缘张裂形成的、处于早期演化阶段的活动性大陆边缘弧后盆地。
The second one depicts research developments in the formation mechanism of continental rifts, pointing out the two major types of rifting, active and passive, and the model of mantle diapire.
综合介绍了关于大陆裂谷形成机制主要分成主动型和被动型两种裂谷作用的基本类型和地幔底辟模型的论点。
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