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Recent Geodetic Results in the Azores Triple Junction Region

机译:亚速尔群岛三结交界处的最新大地测量结果

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GPS (Global Positioning System) observations started to be carried out in the Azores region under the scope of the TANGO (TransAtlantic Network for Geodesy and Oceanography) project in 1988. The measurements carried out between 1993 and 2000 (five campaigns) on nine GPS sites (one per island) were reprocessed using two state–of–the-art software packages. Different methodologies were applied to compute each campaign solution and the derived velocity field. The velocity fields, including the motions of two permanent stations, recently installed in the Azores, were computed within the most recent geodetic reference frame, ITRF2000 (International Terrestrial Reference Frame, solution 2000). They are compared with the motions of the stable rigid tectonic plates using as reference DEOS2k, a global tectonic model developed using geodetic data. The relative motions between the Western and Central groups of islands yield to evaluate the opening rate of the Mid-Atlantic Ridge (boundary between the North American plate and the Eurasian and African plates). Concerning the boundary between the Eurasian and African plates, the motion of the TANGO sites in the Central and Eastern groups clearly identifies the transition pattern between those two plates. Two of the sites are considered to be located in the stable part of these plates, whereas the remaining five are within the deformation region of the Eurasia-Africa boundary. The conclusions are analyzed in view of the different deformation models, derived from geodynamic or geophysical data that have been proposed for the region.
机译:1988年,在TANGO(跨大地测量学和海洋学跨大西洋网络)项目的范围内,开始在亚速尔群岛地区进行GPS(全球定位系统)观测。在1993年至2000年(五个运动)之间对9个GPS站点进行了测量。 (每个岛一个)使用两个最新的软件包进行了重新处理。应用了不同的方法来计算每个战役解决方案和派生的速度场。在最近的大地测量参考系ITRF2000(国际陆地参考系,解决方案2000)中计算了速度场,包括最近在亚速尔群岛中安装的两个永久站的运动。使用DEOS2k作为参考,将其与稳定的刚性构造板块的运动进行比较,DEOS2k是使用大地测量数据开发的全球构造模型。西部和中部岛屿群之间的相对运动可用来评估大西洋中部海脊(北美板块与欧亚大陆板块和非洲板块之间的边界)的开口率。关于欧亚板块与非洲板块之间的边界,中部和东部组的TANGO站点的运动清楚地确定了这两个板块之间的过渡方式。其中两个站点被认为位于这些板块的稳定部分,而其余五个站点位于欧亚大陆-非洲边界的变形区域内。根据不同的变形模型对结论进行了分析,这些模型是从对该地区提出的地球动力学或地球物理数据中得出的。

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