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GOCE satellite derived gravity and gravity gradient corrected for topographic effect in the South Central Andes region

机译:GOCE卫星得出的重力和重力梯度已校正,可用于安第斯中南部地区的地形影响

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摘要

Global gravity field models, derived from satellite measurements integrated with terrestrial observations, provide a model of the Earth’s gravity field with high spatial resolution and accuracy.\udThe Earth Gravity Model EGM08, a spherical harmonic expansion of the geopotential up to degree and order 2159, has been used to calculate two functionals of the geopotential: the gravity anomaly and the vertical gravity gradient applied to the South Central Andes area. The satellite-only field of the highest resolution has been developed with the observations of satellite GOCE, up to degree and order 250. The topographic effect, a fundamental quantity for the downward continuation and validation of satellite gravity gradiometry data, was calculated\udfrom a digital elevation model which was converted into a set of tesseroids. This data is used to calculate the anomalous potential and vertical gravity gradient. In the Southern Central Andes\udregion the geological structures are very complex, but not well resolved. The processing and interpreting of the gravity anomaly and vertical gradients allow the comparison with geological\udmaps and known tectonic structures. Using this as a basis, a few features can be clearly depicted as the contact between Pacific oceanic crust and the Andean fold and thrust belt, the seamount chains over the Oceanic Nazca Plate, and the Famatinian and Pampean Ranges. Moreover the contact between the Rio de la Plata craton and the Pampia Terrain is of great interest, since it represents a boundary that has not been clearly defined until now. Another great lineament, the Valle Fertil-Desaguadero mega-lineament, an expression of the contact between Cuyania and Pampia terranes, can also be clearly depicted. The authors attempt to demonstrate that the new gravity fields can be used for identifying geological features, and therefore serve as useful innovative tools in geophysical exploration.
机译:全球引力场模型源自与地面观测相结合的卫星测量结果,可提供具有高空间分辨率和精度的地球引力场模型。\ ud地球引力模型EGM08,是一种地势的球谐谐波扩展,其度数和阶数为2159,已用于计算地势的两个函数:重力异常和应用于安第斯中南部地区的垂直重力梯度。通过对GOCE卫星的观测,开发了分辨率最高的纯卫星场,其阶数为250。地形效应是向下延伸和验证卫星重力梯度数据的基本量,由数字高程模型,该模型被转换为一组tesseroids。该数据用于计算反常势和垂直重力梯度。在安第斯中部南部南部地区,地质结构非常复杂,但没有很好地解决。重力异常和垂直梯度的处理和解释可以与地质\ udmap和已知的构造结构进行比较。以此为基础,可以清楚地描述一些特征,如太平洋洋壳与安第斯褶皱和逆冲带之间的接触,纳斯卡板块上的海山链以及法马汀山脉和潘庞山脉。此外,里约热内卢克拉通火山口和潘皮亚地形之间的接触引起了极大的兴趣,因为它代表了一个至今尚未明确界定的边界。也可以清楚地描绘出另一种伟大的风格,即瓦尔·费蒂尔·德萨瓜德罗(Valle Fertil-Desaguadero)巨型风格,表达了卡亚尼亚和潘帕亚山脉之间的接触。作者试图证明新的重力场可用于识别地质特征,因此可作为地球物理勘探中有用的创新工具。

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