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THE STUDY OF ESTABLISHING HORIZONTAL VELOCITY AND DEFORMATION MODEL OF SEMI-DYNAMIC DATUM IN TAIWAN AREA

机译:建立台湾地区半动态基准面水平速度和变形模型的研究

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National coordinate system is the foundation of surveying engineering, the establishment and the selection of geodetic datum would directly impact the accuracy of final result. Plate motion will cause earthquakes, volcanic eruptions and other natural disasters. Plate motion especially non-linear motion can also change the relationship between stations in the reference frame. Therefore, a rational and reliable reference frame is needed to ensure the Euclidean integrity quality. Taiwan is located along the bounding of the Eurasian and the Philippine plate, and is therefore a region of non-rigid motion and therefore will shift and rotate in different directions due to the changing stress field. Taiwan's current coordinate system TWD97, which is built by a fixed single term linear model ITRF94.It is not able to precisely model the non-linear motion of the crustal in the Taiwan region. Therefore, Taiwan needs velocity and deformation model to correct the distortion which caused by the crustal motion. This study used five years of Taiwan CORS GPS data to investigate the horizontal velocity field in Taiwan and established the horizontal velocity and deformation model by curve fitting, interpolation and LOWESS method. GNSS; CORS; plate motion; velocity field; deformation model
机译:国家坐标系是测量工程的基础,大地基准的建立和选择将直接影响最终结果的准确性。板块运动将引起地震,火山喷发和其他自然灾害。平板运动,尤其是非线性运动也可以改变参考系中测站之间的关系。因此,需要一个合理可靠的参考系来保证欧几里得的完整性。台湾位于欧亚大陆和菲律宾板块的边界,因此是非刚性运动的区域,因此由于应力场的变化,它将沿不同的方向移动和旋转。由固定的单项线性模型ITRF94构建的台湾当前坐标系TWD97,无法精确建模台湾地区地壳的非线性运动。因此,台湾需要速度和变形模型来校正由地壳运动引起的变形。本研究利用台湾CORS GPS的5年数据对台湾的水平速度场进行了研究,并通过曲线拟合,插值和LOWESS方法建立了水平速度和变形模型。 GNSS; CORS;板块运动速度场变形模型

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