2021
DOI: 10.1029/2020jb021187
|View full text |Cite
|
Sign up to set email alerts
|

Heterogeneous Interseismic Coupling Along the Xianshuihe‐Xiaojiang Fault System, Eastern Tibet

Abstract: The 1400 km-long left-lateral strike-slip Xianshuihe-Anninghe-Zemuhe-Xiaojiang fault system (XXFS) is one of the largest faults cutting through eastern Tibet and contributing its eastward motion (e.g., Allen et al., 1991;Tapponnier et al., 2001;Tapponnier & Molnar, 1977). East of the Tibetan Plateau, the XXFS extends across the Sichuan and Yunnan provinces and merges with the Red River fault (Figure 1). The XXFS has been one of the most seismically active faults in mainland China, as attested by a detailed his… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

3
25
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
7

Relationship

1
6

Authors

Journals

citations
Cited by 44 publications
(28 citation statements)
references
References 56 publications
3
25
0
Order By: Relevance
“…(c) Interseismic coupling along the MAF from Li et al. (2021). Dark gray dots represent background micro‐seismicity (2009–2019) within 5 km of each side of the fault.…”
Section: Resultsmentioning
confidence: 99%
See 3 more Smart Citations
“…(c) Interseismic coupling along the MAF from Li et al. (2021). Dark gray dots represent background micro‐seismicity (2009–2019) within 5 km of each side of the fault.…”
Section: Resultsmentioning
confidence: 99%
“…The interseismic GPS data allow us to resolve the large-scale locked asperities surrounding the seismic region of the Luding earthquake. Refer to Li et al (2018Li et al ( , 2021 for details of methods related to the block modeling.…”
Section: Interseismic Fault Coupling Shear Stress Rate and The 2022 L...mentioning
confidence: 99%
See 2 more Smart Citations
“…where s is the free slip rate and s c represents the creeping part of the non-fully coupled fault. Based on negative dislocation theory (Matsu'ura et al, 1986), the locking degrees of faults can be obtained by the inversion of surface deformation on each patch and used to estimate the seismic risk of the fault (Jiang et al, 2015;Zhao et al, 2020;Li et al, 2021a;Li et al, 2021b;Jian et al, 2022;Li et al, 2022). Although the coupling fraction has been widely used in the interseismic period, questions remain regarding the coexistence of locking and creeping mechanisms, and the correlation between the coupling fraction and locking depth, because of the lack of a physical model.…”
Section: Introductionmentioning
confidence: 99%