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A MECHANISM FOR DECOUPLING WITHIN THE OCEANIC LITHOSPHERE REVEALED IN THE TROODOS OPHIOLITE

机译:在斜背蛇绿岩中揭示的岩石岩石球内部解耦机制

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Contrasting kinematic histories recorded in the sheeted dykes and underlying plutonic rocks of the Troodos ophiolite provide a new perspective on the mechanical evolution of oceanic spreading centres. The kinematic framework of the decoupling zone that partitions deformation between the sheeted dykes and plutonics contrasts with low-angle detachment models for slow-spreading ridges based on continental-rift analogues. A model for the generation of multiple, horizontal decoupling horizons, linked by planar normal faults, demonstrates new possibilities for the kinematic and rheological significance of seismic reflectors in oceanic lithosphere. [References: 61]
机译:Troodos蛇绿岩的薄片状堤坝和下伏的火山岩中记录的不同运动学历史为海洋扩散中心的机械演化提供了新的视角。分离片状堤坝和岩体之间变形的解耦带的运动学框架与基于大陆裂谷类似物的慢速扩张脊的低角度分离模型形成对比。由平面法向断层链接的多个水平解耦层位生成模型为海洋岩石圈地震反射层的运动学和流变学意义证明了新的可能性。 [参考:61]

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