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Jiali Fault

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Journal Article
Published: 01 April 2020
Seismological Research Letters (2020) 91 (3): 1776–1780.
...Hu Wang; Kaijin Li; Lichun Chen; Xingqiang Chen; An Li Abstract Most active block boundary faults within the Tibetan plateau have been thought of as Holocene active, and are able to produce large earthquakes. However, it is unknown whether the Jiali fault (JLF) has been seismically active...
FIGURES | View All (4)
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Geological structure map: F1, Jiali fault zone; F2, Nujiang fault zone; F3, Yarlung Zangbo River fault zone. Source: the faults and strata are from the China Geological Survey (https://www.ngac.org.cn).
Published: 25 July 2024
Fig. 3. Geological structure map: F1, Jiali fault zone; F2, Nujiang fault zone; F3, Yarlung Zangbo River fault zone. Source: the faults and strata are from the China Geological Survey ( https://www.ngac.org.cn ).
Journal Article
Journal: Geology
Published: 01 August 1998
Geology (1998) 26 (8): 691–694.
... in the Himalayas and southern Tibet, and right-lateral strike slip on the Karakorum-Jiali fault zone can all result from basal shear caused by the Indian plate sliding obliquely beneath Tibet along a gently dipping, arcuate plate boundary. Within the framework of this mechanism, the normal faults in the Himalayas...
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(A) Simplified tectonic map of the Himalaya and Tibetan Plateau showing major tectonic domains. Suture zones and faults: ALT—Altyn Tagh fault; BNS—Bangong–Nujiang suture; IYZS—Indus–Yarlung–Zangbo suture; JF—Jiali fault; JS—Jinshajiang suture; KF—Kunlun fault; KLF—Karakoram fault. (B) Simplified geological map of the Lhasa block (after Kapp et al., 2005). LMF—Luobadui–Milashan fault; SNMZ—Shiquan River–Nam Tso mélange zone.
Published: 08 April 2020
Figure 1. (A) Simplified tectonic map of the Himalaya and Tibetan Plateau showing major tectonic domains. Suture zones and faults: ALT—Altyn Tagh fault; BNS—Bangong–Nujiang suture; IYZS—Indus–Yarlung–Zangbo suture; JF—Jiali fault; JS—Jinshajiang suture; KF—Kunlun fault; KLF—Karakoram fault. (B
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Active tectonic map of the study area and the surface rupture zones induced by the earthquake (revised after [62]). (b, c) Images before and after landslides in the study area. MX-WC Fault: Maoxian-Wenchuan Fault; YX-BC Fault: Yingxiu-Beichuan Fault; PZ-GX: Pengzhou-Guanxian Fault; ATF: Altyn Tagh Fault; HF: Haiyuan Fault; JLF: Jiali Fault; NC: North China block; RRF: Longmenshan thrust belt; KF: Kunlun Fault; SCB: South China block; XF: Xianshuihe Fault.
Published: 01 February 2022
: Altyn Tagh Fault; HF: Haiyuan Fault; JLF: Jiali Fault; NC: North China block; RRF: Longmenshan thrust belt; KF: Kunlun Fault; SCB: South China block; XF: Xianshuihe Fault.
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Figure 3. Schematic lithospheric section of central Tibetan Plateau with deformation structures inferred from receiver function imaging (Fig. DR6; see footnote 1). SQD—southern Qiangtang detachment; BJF—Bengco-Jiali fault; BNS—Bangong-Nujiang suture; ILM—Indian lithospheric mantle; TLM—Tibetan lithospheric mantle.
Published: 01 March 2004
Figure 3. Schematic lithospheric section of central Tibetan Plateau with deformation structures inferred from receiver function imaging (Fig. DR6; see footnote 1). SQD—southern Qiangtang detachment; BJF—Bengco-Jiali fault; BNS—Bangong-Nujiang suture; ILM—Indian lithospheric mantle; TLM—Tibetan
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Topography of the eastern Himalayan syntaxis (EHS) and surrounding regions. The black triangle (LSA station) and blue triangles denote the stations used in this study; the red stars represent earthquakes (Ms≥6.0) occurred since 1900 (see Data and Resources). The black and gray lines denote the major tectonic boundaries and faults, respectively. The inset map illustrates the regional tectonic settings. Abbreviations are as follows: BB‐LLF, Bianba‐Luolong fault; BNS, Bangong‐Nujiang suture; HT, Himalayan Terrane; ITS, Indus‐Tsangpo suture; JLF, Jiali fault; LT, Lhasa Terrane; MLF, Mainling fault; MTF, Motuo fault; and QT, Qiangtang Terrane.
Published: 08 April 2024
and gray lines denote the major tectonic boundaries and faults, respectively. The inset map illustrates the regional tectonic settings. Abbreviations are as follows: BB‐LLF, Bianba‐Luolong fault; BNS, Bangong‐Nujiang suture; HT, Himalayan Terrane; ITS, Indus‐Tsangpo suture; JLF, Jiali fault; LT, Lhasa
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Tectonic sketch map of Southeast Asia (modified after Gilley et al. 2003, Palin et al. 2013). Abbreviations: J.L.F., Jiali Fault; G.F.Z., Gaoligong Fault zone; S.F., Sagaing Fault; W.C.F., Wang Chao Fault; T.P.F., Three Pagodas Fault; R.F., Ranong Fault. The four metamorphic massifs located along the Ailao Shan-Red River shear zone are Xuelong Shan (XLS), Diancang Shan (DCS), Ailao Shan (ALS), and Day Nui Con Voi (DNCV). The inset map shows major Cenozoic faults in Asia (modified from Tapponnier et al. 1990).
Published: 07 February 2022
Fig. 1. Tectonic sketch map of Southeast Asia (modified after Gilley et al . 2003 , Palin et al . 2013 ). Abbreviations: J.L.F., Jiali Fault; G.F.Z., Gaoligong Fault zone; S.F., Sagaing Fault; W.C.F., Wang Chao Fault; T.P.F., Three Pagodas Fault; R.F., Ranong Fault. The four metamorphic
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Tectonic setting of east Kunlun to the Qaidam Basin transition zone and distribution of MT observation points. (a) Tectonic setting. The thick yellow arrows denote the direction of the regional stress: ATF, Altyn Tagh Fault; KLF, East Kunlun Fault; HYF, Haiyuan Fault; RRF, Red River Fault; XXF, Xianshuihe-Xiaojiang Fault; and JLF, Jiali Fault. (b) East Kunlun-Qaidam Basin geologic map. The triangles display the MT observation sites; the red triangles are the profile that we study in this paper: SQDF, South Qaidam Fault. (c) Previous isotropic inversion result. The direction of the profile is from the southwest to the northeast (Xiao et al., 2018).
Published: 11 November 2021
Fault; XXF, Xianshuihe-Xiaojiang Fault; and JLF, Jiali Fault. (b) East Kunlun-Qaidam Basin geologic map. The triangles display the MT observation sites; the red triangles are the profile that we study in this paper: SQDF, South Qaidam Fault. (c) Previous isotropic inversion result. The direction
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(a) Tectonic sketch map of the study area. ITS: Indus–Tsangpo suture; BNS: Bangong–Nujiang suture; LSLS: Longmu–Shuanghu–Lancangjiang suture; JSJS: Jinshajiang suture; ANMQS: A’nyemaqen suture; MFT: main frontal thrust; LMST: Longmenshan thrust; KKF: Karakorum fault; SGF: Sagaing fault; JLF: Jiali fault; ARF: Ailao Shan–Red River fault; YXAZXF: Yushu–Xianshuihe–Anninghe–Zemuhe–Xiaojiang fault; SQLF: south Qilian fault [27, 28, 32]. (b) Geological map of the study area. (c) A–B geologic profile. (d, e) Photographs of western boundary fault outcrops of the Jinshajiang suture near the town of Boluo.
Published: 12 April 2022
; JLF: Jiali fault; ARF: Ailao Shan–Red River fault; YXAZXF: Yushu–Xianshuihe–Anninghe–Zemuhe–Xiaojiang fault; SQLF: south Qilian fault [ 27 , 28 , 32 ]. (b) Geological map of the study area. (c) A–B geologic profile. (d, e) Photographs of western boundary fault outcrops of the Jinshajiang suture near
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Six strong earthquakes and their focal mechanisms that occurred around boundaries of the Bayankala block after the year 2000. Stars represent the Hoh Xil, Yutian, Wenchuan, and Yushu earthquakes; circles, two additional earthquakes; thick white lines edged with black, boundaries of the Bayankala block (modified from Diao et al., 2010); and dashed rectangles, study regions selected for seismicity analysis. Black lines are main faults: ATF, Altyn Tagh fault; KLF, Kunlun fault; XSF, Xianshuihe fault; LF, Longmenshan fault; JLF, Jiali fault; KRF, Karakorum fault. The color version of this figure is available only in the electronic edition.
Published: 01 October 2012
of the Bayankala block (modified from Diao et al. , 2010 ); and dashed rectangles, study regions selected for seismicity analysis. Black lines are main faults: ATF, Altyn Tagh fault; KLF, Kunlun fault; XSF, Xianshuihe fault; LF, Longmenshan fault; JLF, Jiali fault; KRF, Karakorum fault. The color version
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Tectonic framework of the Himalayan-Tibetan orogen and its adjacent areas. (A) Tectonic framework of the Tibetan Plateau, showing the study area in the eastern Gangdese belt, near the Eastern Himalayan Syntaxis (Yin and Harrison, 2000). (B) The watershed map of the Linzhi region of the Eastern Himalayan Syntaxis of southern Tibet, showing that the collected orbicule boulder was most likely derived from the Gangdese batholith in the Linzhi region. BNS—Bangong-Nujiang suture; IYS—Indus-Yarlu Tsangpo suture; JLF—Jiali fault; JSS—Jinsha suture; LST—Longmen Shan thrust; MBT—Main Boundary thrust; XSF—Xianshuihe fault.
Published: 23 March 2023
of the Eastern Himalayan Syntaxis of southern Tibet, showing that the collected orbicule boulder was most likely derived from the Gangdese batholith in the Linzhi region. BNS—Bangong-Nujiang suture; IYS—Indus-Yarlu Tsangpo suture; JLF—Jiali fault; JSS—Jinsha suture; LST—Longmen Shan thrust; MBT—Main Boundary
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Tectonic setting of the Motuo fault. (a) Simplified fault map of the Namche Barwa syntaxis that belongs to the eastern syntaxis (ES) of the Tibetan plateau (after Harrison and Yin, 2009; Yin and Harrison, 2011; Xie, 2018). Thin red lines show active faults, whereas, thick red lines show strands of the Motuo fault (MTF). Blue lines represent the Yarlung Zangbo River. Red and white solid circles with different sizes denote historic, instrumental record earthquakes and towns. (b) Tectonic location of study area. Cb, Chayu block; JLF, Jiali fault; Lb, Lhasa block; MBT, Main Boundary Thrust; MCT, Main Central thrust; MLF, Milin fault. The color version of this figure is available only in the electronic edition.
Published: 03 March 2021
lines show strands of the Motuo fault (MTF). Blue lines represent the Yarlung Zangbo River. Red and white solid circles with different sizes denote historic, instrumental record earthquakes and towns. (b) Tectonic location of study area. Cb, Chayu block; JLF, Jiali fault; Lb, Lhasa block; MBT, Main
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Tectonic background of the Tibetan plateau and its surrounding areas. The red rectangle represents the present study area. The red star denotes the 22 May 2021 Mw 7.4 Maduo earthquake. The thin black lines represent the boundaries of active blocks (Zhang et al., 2003). The thick black line represents the boundary between the Indian and Eurasian plates (Hasterok et al., 2022). ATF, Altun Tagh fault; AXB, Alxa block; AZF, Anninghe‐Zemuhe fault; BHB, Bayan Har block; CDDB, ChuanDian Diamond block; DXB, Dianxi block; EKLF, East Kunlun fault; GYXF, Garze‐Yushu‐Xianshuihe fault; HMTB, Himalayan main thrust belt; JLF, Jiali fault; JRF, Jinsha River‐Red River fault zone; LMSF, Longmenshan fault zone; LSB, Lhasa block; QDB, Qaidam block; QTB, Qiangtang block; QLB, Qilian block; SCB, South China block; and TRB, Tarim basin.
Published: 15 April 2025
fault; HMTB, Himalayan main thrust belt; JLF, Jiali fault; JRF, Jinsha River‐Red River fault zone; LMSF, Longmenshan fault zone; LSB, Lhasa block; QDB, Qaidam block; QTB, Qiangtang block; QLB, Qilian block; SCB, South China block; and TRB, Tarim basin.
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(A) Sketch map of the Tibetan Plateau and adjacent areas. (B) Geological map of the North Qiangtang block in the Qamdo area and the surrounding North Lancangjiang tectonic belt and Jinshajiang suture. Abbreviations are as follows: JS—Jinshajiang suture; BNS—Bangong Co–Nujiang suture; SMS—Song Ma suture; CMS—Changning-Menglian suture; IS—Inthanon suture; YS—Yalong-Zangpo suture; TS—Tanymas suture; RPS—Rushan–Pshart suture; ShS—Shyok suture; KKF—Karakorum fault; LF—Longmu Co fault; JF—Jiali fault; RRF—Red River fault. Time periods: J-K—Jurassic–Cretaceous; T—Triassic; C1—Carboniferous; Pz—Paleozoic.
Published: 13 February 2019
; SMS—Song Ma suture; CMS—Changning-Menglian suture; IS—Inthanon suture; YS—Yalong-Zangpo suture; TS—Tanymas suture; RPS—Rushan–Pshart suture; ShS—Shyok suture; KKF—Karakorum fault; LF—Longmu Co fault; JF—Jiali fault; RRF—Red River fault. Time periods: J-K—Jurassic–Cretaceous; T—Triassic; C 1
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Surface ruptures of the Wenchuan Mw 7.9 earthquake, China, and earthquake‐induced landslides. (a) Landslide area distribution; (b) landslide point distribution (line A–B is a topographic profile shown in Fig. 5). Inset shows location of the Longmenshan (dark rectangle) and major faults in region. Average directions of block motions, dark arrows. Surface ruptures are revised from Xu et al. (2008) and Xu, Wen, Yu, et al. (2009). Altyn Tagh fault, ATF; Haiyuan fault, HF; Kunlun fault, KF; Jiali fault, JLF; Jiangyou‐Guanxian fault, JGF; Qinchuan fault, QCF; Peng‐guan fault, PGF; Wenchuan‐Maoxian fault, WMF; Beichuan‐Yingxiu fault, BYF. The color version of this figure is available only in the electronic edition.
Published: 01 August 2013
faults in region. Average directions of block motions, dark arrows. Surface ruptures are revised from Xu et al. (2008) and Xu, Wen, Yu, et al. (2009) . Altyn Tagh fault, ATF; Haiyuan fault, HF; Kunlun fault, KF; Jiali fault, JLF; Jiangyou‐Guanxian fault, JGF; Qinchuan fault, QCF; Peng‐guan fault
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(A) Schematic structural map of SE Asia. Several continental-scale shear zones or metamorphic belts outcrop in this region: the Gaoligong shear zone (GLSZ), Chongshan shear zone (CSSZ), Ailao Shan–Red River shear zone (ALRRSZ), Mogok metamorphic belt (MMB), Wangchao and Jiali faults (WCF and JLF)). (B) Topography, major Cenozoic fault systems, and rivers in the Shan Plateau (after Shi et al., 2018). Black arrows indicate the sites of hairpin drainage loops on the Salween and Mekong Rivers. DYJF—Dayingjiang fault, LRF—Longling-Ruili fault, WDF—Wanding fault, NTHF—Nantinghe fault, MLF—Menglian fault, JHF—Jinghong fault, MXF—Mengxing fault, EHS—eastern Himalayan syntaxis, NMF—Nam Ma fault, MCF—Mae Chan fault, DBPF—Dien Bien Phu fault.
Published: 29 August 2019
Figure 1. (A) Schematic structural map of SE Asia. Several continental-scale shear zones or metamorphic belts outcrop in this region: the Gaoligong shear zone (GLSZ), Chongshan shear zone (CSSZ), Ailao Shan–Red River shear zone (ALRRSZ), Mogok metamorphic belt (MMB), Wangchao and Jiali faults
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(A, B) Tectonic reconstruction and evolution of SE Asia. Two sets of conjugate fault systems might have formed within the Shan Plateau in the early stage of India-Asia continental collision. As the eastern Himalayan syntaxis (EHS) passed by, the Shan Plateau would have gradually transitioned from normal to oblique convergence. Regional stress field changed from approximately NE-SW horizontal shortening to E-W–directed extension. Sinistral transtension initiated diachronously along the preexisting structures, coincident with clockwise rotation of upper-crustal fragments under the drag force imposed by the continuing northward advance of the eastern Himalayan syntaxis. MMB—Mogok metamorphic belt, GLSZ—Gaoligong shear zone, ALRRSZ—Ailao Shan–Red River shear zone, RRF—Red River fault, JLF—Jiali fault, SGF—Sagaing fault.
Published: 29 August 2019
force imposed by the continuing northward advance of the eastern Himalayan syntaxis. MMB—Mogok metamorphic belt, GLSZ—Gaoligong shear zone, ALRRSZ—Ailao Shan–Red River shear zone, RRF—Red River fault, JLF—Jiali fault, SGF—Sagaing fault.
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Figure 1. Schematic tectonic map of the Tibetan plateau and adjacent areas showing the main longitudinal river systems and associated depositional basins. (1) Indus River submarine fan; (2) Bengal Bay submarine fan; (3) Salween and Irrawaddy River delta; (4) Mekong River delta; (5) Red River submarine fan; (6) Yangtze River delta; (7) Yellow River delta; (8) Lanzhou basin; (9) Qinghai Lake; (10) Qaidam basin; (11) Tarim basin; (12) Aral Sea; (13) Baluchistan basin; (14) Ganges basin; (15) Badanjilin desert. ATF—Altyn Tagh fault; EKF—East Kunlun fault; KRF—Karakash fault; KKF—Karakorum fault; RRF—Red River fault; SGF—Sagaing fault; CMF—Chaman fault; XXF—Xianshuihe-Xiaojiang fault; JLF—Jiali fault.
Published: 01 March 2006
; RRF—Red River fault; SGF—Sagaing fault; CMF—Chaman fault; XXF—Xianshuihe-Xiaojiang fault; JLF—Jiali fault.
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Geologic maps of (A) the Himalayan-Tibetan orogen; (B) the easternmost Himalayan orogen and southeastern Tibetan Plateau (modified from Webb et al., 2017); and (C) the northern Indo-Burma Ranges compiled from Ding et al. (2001) and Haproff et al. (2018). Abbreviations: EHS—eastern Himalayan syntaxis; GHC—Greater Himalayan Crystalline Complex; IYSZ—Indus-Yarlung suture zone; JF—Jiali fault; LHS—Lesser Himalayan Sequence; LPC—Lohit Plutonic Complex; MBT—Main Boundary thrust; MCT—Main Central thrust; MFT—Main Frontal thrust; STD—South Tibetan detachment; THS—Tethyan Himalayan Sequence.
Published: 09 April 2019
Himalayan syntaxis; GHC—Greater Himalayan Crystalline Complex; IYSZ—Indus-Yarlung suture zone; JF—Jiali fault; LHS—Lesser Himalayan Sequence; LPC—Lohit Plutonic Complex; MBT—Main Boundary thrust; MCT—Main Central thrust; MFT—Main Frontal thrust; STD—South Tibetan detachment; THS—Tethyan Himalayan Sequence.