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Processing, modeling and interpretation of wide-angle seismic data of an active plate boundary, south of Cyprus

机译:处理,建模和解释塞浦路斯南部活动板块边界的广角地震数据

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摘要

Cyprus lies at the southern edge of the Aegean-Anatolian microplate, caught in the convergence of Africa and Eurasia. Subduction of the African plate below Cyprus has probably ceased and this has been attributed to the docking of the Eratosthenes Seamount microcontinental fragment on the northern edge of the African plat in the subduction zone. In early 2010, on R.V. Maria S. Merian, we conducted a wide-angle seismic survey to test the hypothesis that the Hecataeus Ridge, another possible microcontinental block lying immediately offshore SE Cyprus, might be related to an earlier docking event. The upper crust of southern Cyprus is dominated by ophiolites, with seismic velocities of up to 7 km s⁻¹. A wide-angle seismic profile along Hecataeus Ridge was populated with 15 Canadian and German ocean-bottom seismometers at 5 km intervals and these recorded shots from a 6000 cu. in. air gun array, fired approximately every 100 m. Rough topography of the seabed has made picking of phases and their modeling a demanding task. Bandpass and coherency filtering have enabled us to pick phases out to around 80 km. Tomographic inversion of short-range first arrivals provided an initial model of the shallow sub- seabed structure. Forward modeling by ray-tracing, using the code of Zelt and Smith, was then used to model crustal structure down to depths of around 25 km, with no evidence of reflections from Moho. Modeling results provide good control on P-wave velocities in the top 20 km and some indications of deeper events. There is no evidence of true velocities approaching 7 km.s⁻¹ in the top 20 km below the Ridge that might indicate the presence of ophiolitic rocks. Regional gravity and magnetic field data tend to support this proposition. We thus conclude that Hecataeus Ridge is not composed of characteristically ophiolitic, Cyprus (upper plate) crust, and most likely it might be derived from the African (lower) plate.
机译:塞浦路斯位于爱琴海-安纳托利亚微孔板的南部边缘,陷入非洲和欧亚大陆的交汇处。塞浦路斯以下非洲板块的俯冲可能已经停止,这归因于埃拉托森海山微大陆碎片对接在非洲板块北缘的俯冲带。在2010年初,在R.V.玛丽亚·梅里安(Maria S. Merian),我们进行了一次广角地震勘测,以检验以下假设:赫卡特里斯海岭(Hecataeus Ridge)(可能位于塞浦路斯东南部附近的另一个微洲块体)可能与较早的对接事件有关。塞浦路斯南部的上地壳以蛇绿岩为主,地震速度高达7 kms⁻¹。沿Hecataeus脊的广角地震剖面以15公里的间隔装有5台加拿大和德国海底地震仪,并记录了6000立方米的镜头。空气喷枪阵列,大约每100 m发射一次。海底的崎ography地形使选择相及其建模成为一项艰巨的任务。带通和相干性过滤使我们能够选择约80 km的相位。短程首次到达的层析成像反演提供了浅海底海床结构的初始模型。然后,使用Zelt和Smith的代码通过射线追踪进行正向建模,然后对地壳结构进行建模,直到深度约25 km,而没有Moho反射的证据。模拟结果很好地控制了前20 km的纵波速度,并提供了一些更深层事件的迹象。没有证据表明在山脊以下20 km的顶部,真实速度接近7 km.s -1,这可能表明存在石质岩。区域重力和磁场数据倾向于支持这一观点。因此,我们得出的结论是,Hecataeus Ridge不是由特征性的卵石塞浦路斯(上板)壳构成的,很可能它可能来自非洲(下板)板。

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    Rahimi Ayda;

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