Structural Deformation Style and Seismic Potential of the Maoyaba Fault, Southeastern Margin of the Tibet Plateau Article Swipe
Zhang Xianbing
,
Ning Zhong
,
Xiaopeng Yu
,
Guifang Yang
,
Haibing Li
·
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.3390/rs17071288
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.3390/rs17071288
The southeastern margin of the Tibet Plateau represents one of the most seismically active zones in China and serves as a natural laboratory for investigating the uplift dynamics and lateral expansion mechanisms of the plateau. The Litang fault zone (LTFZ) lies within the northwest Sichuan sub-block on the southeastern margin of the Tibet Plateau, running almost parallel to the Xianshuihe fault zone and forming a V-shaped conjugate structure system with the Batang fault zone (BTFZ). The Maoyaba fault (MYBF) is a significant component of the northwestern part of the LTFZ, exhibiting activity in the late Quaternary. It triggered the ancient Luanshibao landslide and caused the Litang earthquake in 1729 AD, demonstrating intense seismic activity. Employing high-resolution remote sensing interpretation, field surveys, UAV photogrammetry, and UAV LiDAR, this study further examines the geometric distribution and kinematic properties of the MYBF, as well as paleoearthquake events recorded by the fault scarps. Combined with the geometric distribution and kinematic properties of the Hagala fault (HGLF) and Zimeihu fault (ZMHF), this study discusses the late Quaternary structural deformation style and seismic potential of the MYBF. The MYBF could produce earthquakes of approximately Mw 6.7 ± 0.3, with an average co-seismic slip of about 0.68 m and an average recurrence interval of strong earthquakes since the late Quaternary ranging from 0.9 to 1.1 ky. The likelihood of surface rupture earthquakes occurring in the near future is low; however, the expansion of the HGLF could induce moderate to strong earthquakes in the MYB area. The variation in the local tectonic stress field, which is influenced by the Litang–Batang V-shaped structure system and lithological differences, results in the formation of an extensional horsetail structure in the northwestern segment of the LTFZ. Both the HGLF and ZMHF remain active faults. Under the influence of nearly north–south tensile stress, these faults and the Litang–Batang V-shaped structure system collectively regulate the movement of regional crustal material.
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- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.3390/rs17071288
- https://www.mdpi.com/2072-4292/17/7/1288/pdf?version=1743742798
- OA Status
- gold
- References
- 45
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4409171709
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- OpenAlex ID
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https://openalex.org/W4409171709Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.3390/rs17071288Digital Object Identifier
- Title
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Structural Deformation Style and Seismic Potential of the Maoyaba Fault, Southeastern Margin of the Tibet PlateauWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
-
2025Year of publication
- Publication date
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2025-04-04Full publication date if available
- Authors
-
Zhang Xianbing, Ning Zhong, Xiaopeng Yu, Guifang Yang, Haibing LiList of authors in order
- Landing page
-
https://doi.org/10.3390/rs17071288Publisher landing page
- PDF URL
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https://www.mdpi.com/2072-4292/17/7/1288/pdf?version=1743742798Direct link to full text PDF
- Open access
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YesWhether a free full text is available
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goldOpen access status per OpenAlex
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https://www.mdpi.com/2072-4292/17/7/1288/pdf?version=1743742798Direct OA link when available
- Concepts
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Geology, Margin (machine learning), Seismology, Plateau (mathematics), Fault (geology), Deformation (meteorology), Oceanography, Mathematical analysis, Machine learning, Mathematics, Computer scienceTop concepts (fields/topics) attached by OpenAlex
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