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Xiaojiang Fault

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Journal Article
Published: 02 July 2024
Seismological Research Letters (2024) 95 (6): 3681–3695.
... weighting scheme can effectively reduce the overall travel‐time residual by 7%. The weighted data were then used in the double‐difference tomography method to invert for the crustal velocity structure of the Anninghe–Xiaojiang fault zone. The resulting new model exhibits a lateral resolution of up to 0.25...
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Journal Article
Published: 16 June 2022
Seismological Research Letters (2022) 93 (5): 2484–2497.
...Tian Feng; Miao Zhang; Lisheng Xu; Jianping Wu; Lihua Fang Abstract The left‐lateral strike‐slip Xiaojiang fault is an important tectonic boundary between Sichuan–Yunnan diamond block and the Yangtze block, which accommodated several M > 7.0 damaging earthquakes in the past ∼500 yr, as well...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 10 February 2021
Lithosphere (2021) 2021 (1): 7866379.
...Peng Guo; Zhujun Han; Shaopeng Dong; Zebin Mao; Nan Hu; Fan Gao; Jiani Li Abstract The Xiaojiang fault zone (XJFZ) is an important part of the Xianshuihe-Xiaojiang fault system, acting as the eastern boundary of the Chuan-Dian block on the southeastern margin of the Tibetan Plateau...
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Journal Article
Published: 17 March 2020
Bulletin of the Seismological Society of America (2020) 110 (3): 1191–1210.
...Jingwei Liu; Lifang Zhang; Yi Du ABSTRACT Seismic hazards in the vicinity of the mid‐northern segment of the Xiaojiang fault zone were estimated from scenario earthquakes. Based on its history of earthquakes and activity data, the whole segment is considered capable of generating large earthquakes...
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Journal Article
Published: 11 April 2018
Seismological Research Letters (2018) 89 (3): 1014–1022.
... the source. The experiment was conducted in the east branch of the Xiaojiang fault (XJF) zone in Xundian County, Yunnan Province, China, and it lasted for one week. The relative velocity ( d v / v ) changes are measured with a precision of ∼ 2.0 × 10 − 3 . Consistent velocity variations ranging from 5% to 20...
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Series: GSA Special Papers
Published: 01 January 1998
DOI: 10.1130/0-8137-2327-2.1
Series: GSA Special Papers
Published: 01 January 1998
DOI: 10.1130/SPE327
Image
Fault rupture scenarios for the mid‐northern segment of the Xiaojiang fault zone. S1, Qiaojia–Menggu segment; S2, Menggu–Awang segment; S3, Gongshan–Xiaoxinjie segment; S4, Xiaoxinjie–Xujiadu segment; S5, east Yiliang segment; S6, Daduo–Cangxi segment; and S7, Cangxi–Chengjiang segment.
Published: 17 March 2020
Figure 4. Fault rupture scenarios for the mid‐northern segment of the Xiaojiang fault zone. S1, Qiaojia–Menggu segment; S2, Menggu–Awang segment; S3, Gongshan–Xiaoxinjie segment; S4, Xiaoxinjie–Xujiadu segment; S5, east Yiliang segment; S6, Daduo–Cangxi segment; and S7, Cangxi–Chengjiang segment.
Image
(a) Map view of the entire Xiaojiang fault. The blue stars mark M ≥ 6.5 historical large earthquakes. The double purple circles show the locations of cities. The magenta lines denote the entire Xiaojiang fault, and the black lines represent other faults. DLSF, Daliangshan fault; HHF, Honghe fault; LFF, Lianfeng fault; PDHF, Puduhe fault; XJF, Xiaojiang fault; ZMHF, Zemuhe fault; and ZTF, Zhaotong fault. The background is colored by topography, and the color bar is shown on the left of the figure. The range bounded by three pairs of the black arrows at the top of panel (a) denotes the northern, middle, and southern section of the Xiaojiang fault zone, respectively, from left to right. The range bounded by the red arrows denotes the middle‐northern section of the Xiaojiang fault zone, which is shown in panel (b). (b) Map view of the study region. The red circles denote earthquakes obtained by machine learning‐based earthquake location workflow (LOC‐FLOW) and further relocated by tomoDD (from November 2019 to November 2020), and crosses denote inversion grids for the 3D velocity model. The green stars show the epicenters of the three largest earthquakes (the 15 January 2020 ML 4.4 Xundian earthquake, the 18 May 2020 ML 5.1 Qiaojia earthquake, and the 8 July 2020 ML 4.6 Dongchuan earthquake) during our study period. The light blue triangles represent the distribution of the Qiaojia temporary seismic array, and the black triangles represent permanent stations. The inset shows regional map of southeast Asia, with the blue rectangle indicating the study region (panel b). SB, Sichuan basin; SGB, Songpan–Ganzi block; SYDB, Sichuan–Yunnan diamond block; and YZB, Yangtze block. The color version of this figure is available only in the electronic edition.
Published: 16 June 2022
Figure 1. (a) Map view of the entire Xiaojiang fault. The blue stars mark M ≥ 6.5 historical large earthquakes. The double purple circles show the locations of cities. The magenta lines denote the entire Xiaojiang fault, and the black lines represent other faults. DLSF, Daliangshan fault; HHF
Image
(a) A map of the study region surrounding the Xiaojiang fault (XJF). The red solid square denotes the experimental site, which is further enlarged in (b). The black solid lines denote the faults in the region, and the black solid circles denote the epicenters of historical earthquakes. Cities are labeled with circled solid dots. I, South China block; II, Tibetan subblock. (Inset) A larger map of the study region. (b) The detailed distribution of the wells (the hollow circles), the seismic stations (the solid triangles), and the fault zone (the gray band). (c) The vertical seismic profile velocity imaging with long offsets at the east branch of the XJF (from Gang Hu) and the drill hole columnar section of Wells ZK1, ZK3, and ZK4.
Published: 11 April 2018
Figure 1. (a) A map of the study region surrounding the Xiaojiang fault (XJF). The red solid square denotes the experimental site, which is further enlarged in (b). The black solid lines denote the faults in the region, and the black solid circles denote the epicenters of historical earthquakes
Journal Article
Journal: GSA Bulletin
Published: 01 March 2000
GSA Bulletin (2000) 112 (3): 413–423.
...Erchie Wang; B. Clark Burchfiel Abstract From at least 2–4 Ma to present, crust in the southeastern part of the Tibetan Plateau west of the convex-east Xianshuihe-Xiaojiang fault system has deformed internally and rotated clockwise around the eastern Himalayan syntaxis. The northwest-striking Ganzi...
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Image
Seismotectonic setting and distribution map of the Jianshui fault in the southern segment of the Xiaojiang fault zone. (a) Main active faults and large earthquakes with magnitudes of ≥7.0 in the study area. Fault locations and slip senses are simplified from Xu et al. [21]. Red lines represent the Xianshuihe-Xiaojiang left-lateral strike-slip fault system. The rectangular box represents the location of the Jianshui fault. Earthquake locations and magnitudes are from the China Earthquake Information Network. GPS velocity field relative to stable Eurasia is from Liang et al. [22]. Abbreviations: GZF = Ganzi fault; XSHF = Xianshuihe fault; ANHF = Anninghe fault; ZMHF = Zemuhe fault; DLSF = Daliangshan fault; N-XJF = northern segment of the Xiaojiang fault; C-XJF = central segment of the Xiaojiang fault; S-XJF = southern segment of the Xiaojiang fault; JSF = Jianshui fault; QJF = Qujiang fault; SPF=Shiping fault; RRF = Red River fault; DBFF = Dien Bien Phu fault; NTHF = Nantinghe fault; LJ-XJHF = Lijiang-Xiaojinhe fault; JSJF = Jinshajiang fault; LTF = Litang fault; LMSF = Longmenshan fault. (b) Google Earth optical image showing the clear linear features of the Jianshui fault. Red arrows represent the location of the fault. (c) Distribution map of the Jianshui fault. The hillshade map is generated from the ASTGTM DEM (30 m resolution).
Published: 10 February 2021
Figure 1 Seismotectonic setting and distribution map of the Jianshui fault in the southern segment of the Xiaojiang fault zone. (a) Main active faults and large earthquakes with magnitudes of ≥7.0 in the study area. Fault locations and slip senses are simplified from Xu et al. [ 21 ]. Red lines
Journal Article
Journal: GSA Bulletin
Published: 01 May 2006
GSA Bulletin (2006) 118 (5-6): 672–688.
...-Xiaojiang fault system, which deflects but does not cut the Red River fault. The distributed nature of the Xianshuihe-Xiaojiang fault system as it approaches the Red River fault is important for accommodating shearing across the strong crustal anisotropy formed by the Red River fault and Ailao Shan shear...
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Journal Article
Journal: Geology
Published: 01 February 1997
Geology (1997) 25 (2): 179–182.
...Robert W. King; Feng Shen; B. Clark Burchfiel; Leigh H. Royden; Erchie Wang; Zhiliang Chen; Yuping Liu; Xuan-Yang Zhang; Ji-Xiang Zhao; Yulin Li Abstract Global Positioning System measurements performed over a 2–4 yr period confirm the Xianshuihe-Xiaojiang fault system as one of the primary active...
Image
Earth models used in this study. (a) The WYUN model for the region to the west of the Sagaing fault. (b) CYUN is the initial model for the region between the Xianshuihe–Xiaojiang fault and Sagaing fault, which includes the Sichuan–Yunnan rhombic block and Indochina. (c) The CUS model is used for the events at the east of the Xianshuihe–Xiaojiang fault system.
Published: 01 November 2010
Figure 2. Earth models used in this study. (a) The WYUN model for the region to the west of the Sagaing fault. (b) CYUN is the initial model for the region between the Xianshuihe–Xiaojiang fault and Sagaing fault, which includes the Sichuan–Yunnan rhombic block and Indochina. (c) The CUS model
Journal Article
Published: 03 January 2025
Bulletin of the Seismological Society of America (2025) 115 (2): 505–515.
... on the reliability and interpretability of the automated measurements. Most fast‐wave polarization directions align with the regional maximum horizontal stress and the nearby fault trends, generally consistent with previous observations. Five stations near the Zemuhe and Xiaojiang faults show a nearly 90° flip...
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Image
Seventy-nine focal mechanisms of small-to-moderate size events in the Yunnan and Sichuan regions. Dark gray triangles are the 25 temporary seismic stations. Four major fault systems are labeled: SF, right-lateral Sagaing fault; RRF, right-lateral Red River fault; XSH–XJF, left-lateral Xianshuihe–Xiaojiang fault; LMS, thrust Longmen Shan fault. SYR stands for the Sichuan–Yunnan rhombic block bounded by the Red River fault and the Xianshuihe–Xiaojiang fault. EHS represents the East Himalayan syntaxis. The inset shows the location of the study area with regional estimated surface motion direction (black arrows) (Royden et al., 2008).
Published: 01 November 2010
Xianshuihe–Xiaojiang fault; LMS, thrust Longmen Shan fault. SYR stands for the Sichuan–Yunnan rhombic block bounded by the Red River fault and the Xianshuihe–Xiaojiang fault. EHS represents the East Himalayan syntaxis. The inset shows the location of the study area with regional estimated surface motion
Journal Article
Published: 10 January 2024
Seismological Research Letters (2024) 95 (3): 1759–1775.
... high‐resolution velocity and resistivity models and geochemical observation results, we can comprehensively understand the medium structure and the seismogenesis in the study area. The results show that the high‐attenuation characteristics in the shallow layer of the Xiaojiang fault zone and the Zemuhe...
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Journal Article
Published: 10 July 2023
Seismological Research Letters (2023) 94 (5): 2384–2396.
... and high V P / V S at depths ranging from 3 to 10 km beneath the Qiaojia area along the Xiaojiang fault (XJF), which suggests that the seismic activity in this area may increase with the storage of the BHT dam in April 2021. * Corresponding author: [email protected] 11 February 2023 ©...
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Journal Article
Published: 03 March 2021
Seismological Research Letters (2021) 92 (4): 2122–2133.
... recorded by dense local seismic stations of the Qiaojia array constructed near the Xiaojiang fault zone. The focal mechanism of the mainshock exhibited strike‐slip motion with a centroid depth of 8 km. We determined the seismogenic fault of the Qiaojia earthquake using aftershock relocation with local...
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