Mini-batch-based joint inversion of surface wave dispersion and gravity anomaly for high-resolution crustal velocity structure of China and its adjacent regions

IF 2.4 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Journal of Asian Earth Sciences Pub Date : 2026-04-01 Epub Date: 2026-01-30 DOI:10.1016/j.jseaes.2026.106983
Aolin Xiong , Jiangtao Li , Yudi Pan , Hanbing Ai
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引用次数: 0

Abstract

High-resolution crustal velocity models are essential for understanding the tectonic evolution of China and its adjacent regions, while inversion based solely on an individual geophysical dataset inherently suffers from uncertainty and limited resolution. To mitigate these limitations, we propose a mini-batch-based joint inversion method that integrates surface wave dispersion and gravity anomaly, and apply it to achieve high-resolution crustal shear-wave velocity structure beneath China and its adjacent regions. We improve the joint inversion framework by Du et al. (2021) through randomly partitioning the surface wave dispersion data into mini-batches, to overcome computation and memory issues with large dataset. Besides, to enhance the sensitivity and constraints of Bouguer gravity anomaly on crustal and uppermost mantle structures, we apply a spherical harmonic expansion to remove long-wavelength background signals. The proposed mini-batch strategy ensures stochastic utilization of the full dataset, significantly reduces computational costs, accelerates convergence, and improves resistance to noise interference. The joint inversion results exhibit apparent improvements in structural resolution, allowing for clearer delineation of segmented low-velocity zones across the Tibetan Plateau, relatively high-velocity anomalies beneath the Lhasa and southern Qiangtang Terrane, stable cratonic features beneath the Sichuan and Tarim Basin, and low-velocity anomalies beneath the Qilian, Changbai and Taiwan orogenic belts. The results also provide refined constraints on the geometry and depth of the Moho interface, demonstrating high sensitivity to complex tectonic regions. These findings provide important constraints on regional tectonic mechanisms. The proposed joint inversion method holds broad application potential in large-scale, massive-data geophysical imaging.

Abstract Image

中国及邻区高分辨率地壳速度结构面波频散与重力异常联合小批反演
高分辨率的地壳速度模型对于了解中国及其邻近地区的构造演化至关重要,而仅基于单个地球物理数据集的反演本身就存在不确定性和分辨率有限的问题。为了克服这些局限性,我们提出了一种结合面波频散和重力异常的小批量联合反演方法,并将其应用于中国及其邻区地壳横波速度结构的高分辨率反演。我们改进了Du等人(2021)的联合反演框架,通过将表面波色散数据随机划分为小批量,以克服大型数据集的计算和内存问题。此外,为了增强布格重力异常对地壳和上地幔结构的敏感性和约束,我们采用了球谐展开法去除长波长背景信号。所提出的小批量策略保证了整个数据集的随机利用,显著降低了计算成本,加快了收敛速度,并提高了对噪声干扰的抵抗力。联合反演结果在构造分辨率上有明显提高,可以更清晰地圈定青藏高原的分段低速带、拉萨和羌塘南地体下的相对高速异常、四川盆地和塔里木盆地下的稳定克拉通特征以及祁连、长白和台湾造山带下的低速异常。结果还提供了对莫霍界面的几何形状和深度的精细约束,显示出对复杂构造区域的高灵敏度。这些发现为研究区域构造机制提供了重要的约束条件。所提出的联合反演方法在大尺度、大数据物探成像中具有广阔的应用潜力。
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来源期刊
Journal of Asian Earth Sciences
Journal of Asian Earth Sciences 地学-地球科学综合
CiteScore
5.90
自引率
10.00%
发文量
324
审稿时长
71 days
期刊介绍: Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review. The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance. The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.
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