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THE CRUSTAL VELOCITY FIELD MOSAIC OF THE ALPINE MEDITERRANEAN AREA: INSIGHT FROM NEW GEODETIC DATA

机译:高山地中海地区的地壳速度场马赛克:来自新的大地测量数据的洞察力

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Geodetic techniques, such as Global Navigation Satellite System (GNSS), Synthetic Aperture Radar (SAR), satellite gravity missions, etc., have made significant contributions in monitoring temporal and spatial changes in Earth's lithosphere and atmosphere. A new crustal velocity field for the Alpine Mediterranean area (Farolfi & Del Ventisette, 2015) was determined by using a time series spanning 6.5 years of GNSS permanent stations. Thus, processing was performed by using state-of-the-art antenna phase center model, new recomputed satellite orbits and a new more accurate tropospheric model. The aim of this work is to calculate and analyze the spatial variations of continuous time series of GNSS permanent stations, to estimate crustal velocities in the Alpine Mediterranean area. The resulting velocity field gives a strong contribution in the framework of the contemporary geodynamics.
机译:诸如全球导航卫星系统(GNSS),合成孔径雷达(SAR),卫星重力任务等的大地测量技术在监测地球岩石圈和气氛中的时间和空间变化方面取得了重大贡献。通过使用6.5年GNSS永久站的时间序列确定了高山地中海地区(Farolfi&Del Ventisette,2015)的新的地壳速度场。因此,通过使用最先进的天线相位模型,新的重新计算卫星轨道和新的更准确的对流层模型来执行处理。这项工作的目的是计算和分析GNSS永久站连续时间序列的空间变化,以估算高山地中海地区的地壳速度。所得到的速度场在当代地球动力学的框架中提供了强烈贡献。

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