Euler-pole clustering of GNSS velocities using unsupervised machine learning in the Southeastern Tibetan Plateau: Crustal block identification and the dominance of sinistral-slip faults

IF 10 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Earth-Science Reviews Pub Date : 2026-05-01 Epub Date: 2026-02-06 DOI:10.1016/j.earscirev.2026.105420
X. Rui , D.S. Stamps
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引用次数: 0

Abstract

Previous studies have constrained fault slip rates and crustal block geometries of the Southeastern Tibetan Plateau (SETP) with contradictory results due to complex geodynamics and deformation patterns as well as subjective choices of crustal block boundaries. In this work, we address the issue of uncertain crustal block geometries by employing an unsupervised machine learning Euler pole clustering algorithm that automatically resolves regions that behave as rigid blocks (clusters) rotating on a sphere using GNSS velocity vectors. Optimal clustering results, determined by F-test and Euler-vector (angular velocity vector) overlap analyses, indicate 4 elongated crustal blocks exist in the SETP that are approximately parallel and delineated by a set of arcuate sinistral-slip faults. Our clustering results redefine the first-order kinematics of the SETP region with new crustal block definitions that elucidate the dominance of sinistral-slip faults.
基于无监督机器学习的青藏高原东南部GNSS速度欧拉极聚类:地壳块体识别和左滑断层的主导地位
由于复杂的地球动力学和变形模式以及对地壳块体边界的主观选择,以往的研究对青藏高原东南部的断层滑动率和地壳块体几何形状进行了约束,但结果相互矛盾。在这项工作中,我们通过采用无监督机器学习欧拉极点聚类算法来解决不确定地壳块几何形状的问题,该算法使用GNSS速度矢量自动解析在球体上旋转的刚性块(簇)区域。通过f检验和欧拉矢量(角速度矢量)重叠分析确定的最优聚类结果表明,SETP中存在4个细长的地壳块体,它们近似平行,由一组弧形的正弦滑动断层所描绘。我们的聚类结果用新的地壳块体定义重新定义了SETP区域的一阶运动学,阐明了左滑断层的主导地位。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Earth-Science Reviews
Earth-Science Reviews 地学-地球科学综合
CiteScore
21.70
自引率
5.80%
发文量
294
审稿时长
15.1 weeks
期刊介绍: Covering a much wider field than the usual specialist journals, Earth Science Reviews publishes review articles dealing with all aspects of Earth Sciences, and is an important vehicle for allowing readers to see their particular interest related to the Earth Sciences as a whole.
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