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Global plate motion models incorporating the velocity field of ITRF96

机译:整合ITRF96速度场的整体板块运动模型

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摘要

In this paper, incorporating the ITRF96 velocity field that is free of any tectonic plate model assumption, a new present-day plate motion model relative to the ITRF96 reference frame, called the ITRF96VEL, is determined. The total angular momentum of all tectonic plates with regards to the ITRF96VEL shows that the ITRF96 rotates in a right-handed sense relative to the no-net-rotation (NNR) reference frame at O.164°/m.yr. about 50.7°S, 65.8°E. This means that ITRF96 is not sufficiently concordant with the definition of the Conventional Terrestrial Reference System (CTRS). In order to more properly compare plate motions from the ITRF96 velocity field with the NNR-NUVEL1A, another plate motion model relative to the NNR reference frame, called the NNR-ITRF96VEL, is also established. The results indicate that the NNR-ITRF96VEL is quite consistent with the NNR-NUVEL1A. The consistency testifies to the reliability of the NNR-NUVEL1A, and shows the tectonic plate motions were steady over past millions of years.
机译:在本文中,结合没有构造板块模型假设的ITRF96速度场,确定了相对于ITRF96参考框架的新的当今板块运动模型,称为ITRF96VEL。关于ITRF96VEL,所有构造板块的总角动量表明,ITRF96相对于无网旋转(NNR)参考系以O.164°/ m.yr的惯性向右旋转。大约50.7°S,65.8°E。这意味着ITRF96与常规陆地参考系统(CTRS)的定义不够充分。为了更正确地比较来自ITRF96速度场的板块运动与NNR-NUVEL1A,还建立了另一个相对于NNR参考系的板块运动模型,称为NNR-ITRF96VEL。结果表明,NNR-ITRF96VEL与NNR-NUVEL1A非常一致。一致性证明了NNR-NUVEL1A的可靠性,并显示了构造板块运动在过去数百万年中是稳定的。

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