Advances in Ocean Plate Motion and Seismic Research

A special issue of Journal of Marine Science and Engineering (ISSN 2077-1312). This special issue belongs to the section "Geological Oceanography".

Deadline for manuscript submissions: 30 June 2025 | Viewed by 992

Special Issue Editors


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Guest Editor
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China
Interests: neotectonics and active tectonics
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Guest Editor
School of Earth Sciences, China University of Geosciences, Wuhan, China
Interests: real-time seismology; induced seismicity; active faults
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Special Issue Information

Dear Colleagues,

The dynamic nature of the Earth's lithosphere, particularly the oceanic plates, plays a crucial role in our understanding of the geophysical and geological processes of the Earth. This Special Issue, titled “Advances in Ocean Plate Motion and Seismic Research”, aims to showcase recent breakthroughs and cutting-edge research in the field of ocean plate tectonics and seismology. This collection includes studies on the mechanisms driving plate motions, the interaction between tectonic plates and underlying mantle processes, and the resulting seismic activities. By integrating observational data, advanced modeling techniques, and innovative analytical approaches, the contributions in this Issue provide new insights into the complex behavior of oceanic plates. Key topics include the assessment of ocean plate boundaries; subduction zone dynamics, mid-ocean ridge processes, and volcanoes; intraplate earthquakes; and tsunamis associated with subduction zones. This Special Issue highlights the importance of multidisciplinary approaches in advancing our understanding of ocean plate motions and their implications for global seismic hazards. In it, researchers, geophysicists, and Earth scientists will find valuable information and novel perspectives that can inform future studies and contribute to the broader field of Earth sciences.

Prof. Dr. Zhonghai Wu
Prof. Dr. Dun Wang
Guest Editors

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Keywords

  • ocean plate boundaries
  • subduction zone dynamics
  • mid-ocean ridge processes
  • intraplate seismicity
  • great earthquake disaster related with subduction zones
  • volcanic activity associated with subduction zones

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Published Papers (1 paper)

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Research

23 pages, 14443 KiB  
Article
The Formation and Modification of the Arcuate Tectonic Belt in the Northeastern Tibetan Plateau: Insight from Three-Dimensional Finite Element Numerical Simulation
by Yilin Zhao, Wei Shi, Yujun Sun and Guiting Hou
J. Mar. Sci. Eng. 2025, 13(1), 170; https://doi.org/10.3390/jmse13010170 - 18 Jan 2025
Viewed by 626
Abstract
The arcuate tectonic belt in the northeast Tibetan Plateau has been a contentious topic regarding its formation and evolution, owing to its distinctive geological structure as the lateral growth boundary of the plateau. In this research, leveraging geological and geophysical data, a three-dimensional [...] Read more.
The arcuate tectonic belt in the northeast Tibetan Plateau has been a contentious topic regarding its formation and evolution, owing to its distinctive geological structure as the lateral growth boundary of the plateau. In this research, leveraging geological and geophysical data, a three-dimensional finite element numerical model is employed to explore the impact of lateral and vertical inhomogeneities in lithospheric strength on the northeast Tibetan Plateau’s growth and the arcuate tectonic belt’s formation and alteration. Additionally, the kinematic and deformation traits of the arcuate tectonic belt, such as regional motion velocity, stress, and crustal thickness during shortening and strike-slip deformation, are comparatively analyzed. The findings indicate that the arcuate tectonic belt takes shape when the weakly strengthened Tibetan Plateau is impelled into the Yinchuan Basin after being obstructed by the robust Alax and Ordos blocks during lateral expansion. Intense shear deformation occurs at the block boundaries during the arc tectonic belt’s formation. The weak middle-lower crust, serving as a detachment layer, facilitates the plateau’s lateral growth and crustal shortening and thickening without perturbing the overall deformation characteristics. It is verified that the arcuate tectonic belt was formed during the NE-SW compression phase from around 9.5 to 2.5 Ma, accompanied by significant crustal shortening and thickening. Since 2.5 Ma, within the ENE-WSW compression process, the internal faults of the arcuate tectonic belt are predominantly strike-slip, with no pronounced crustal shortening and thickening. Only local topographical modification is conspicuous. This study will enhance our comprehension of the Tibetan Plateau’s uplift and lateral growth process and furnish a foundation for investigating the formation of arcuate tectonic belts. Full article
(This article belongs to the Special Issue Advances in Ocean Plate Motion and Seismic Research)
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