The NUVEL1-A is one of the old and popular plate tectonic models. While the NUVEL1-A is a geological-based model, recently a model has been proposed (GSRM2.1 model) which is based on the results of space geodetic techniques. In this work, we investigate the consistency of these models with the VLBI and SLR results in Europe. Direction and magnitude of the horizontal motion from NUVEL-1A and GSRM2.1 models are compared with corresponding values from both geodetic techniques. This comparison provides valuable deductions such as: (1) The values of geodetic-based model (GSRM2.1) show better agreement with SLR and VLBI results (2) In each comparison between geodetic results and modelled values, direction divergence is larger than magnitude difference.

NUVEL1-A 是古老而流行的板块构造模型之一。虽然 NUVEL1-A 是基于地质的模型，但最近提出了一个基于空间大地测量技术结果的模型（GSRM2.1 模型）。在这项工作中，我们调查了这些模型与欧洲 VLBI 和 SLR 结果的一致性。NUVEL-1A 和 GSRM2.1 模型的水平运动方向和幅度与两种大地测量技术的相应值进行了比较。该比较提供了有价值的推论，例如：（1）基于大地测量的模型（GSRM2.1）的值与SLR和VLBI结果具有更好的一致性（2）在大地测量结果和建模值之间的每次比较中，方向发散大于幅度区别。