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Honghe fault system

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Image
Published: 09 January 2018
Figure 1. Fault distributions around the Xichang fault bend, which has an angle of about 30°. Thick and thin lines denote active and inactive faults, respectively. The inset map shows the fault systems of the Tibetan plateau (modified after Tapponnier et al. , 2001 ). The base map is from
Journal Article
Journal: GSA Bulletin
Published: 18 March 2025
GSA Bulletin (2025)
... (Wang et al., 2017). The purple and green shading indicates the modern drainage of the Yellow River and Yangtze River, respectively. The orange shading indicates the Chinese Loess Plateau. (B) ATF Altyn Tagh Fault; HF Haiyuan Fault; LPS Liu Pan Shan Thrust; NQF North Qinling fault system. The growth...
Image
Published: 01 June 2017
showing the location of A in the northeastern Tibetan Plateau. White rectangle shows the location of Figure 2 along the Lenglongling fault. Fault abbreviations: LMSF—Longmenshan fault; AEJF—Altun Tagh fault; DKLF—Dongkunlun fault; XSHF—Xianshui River fault; SGS—Shanxi graben system; HHF—Honghe fault.
Image
Published: 19 September 2023
, Longmenshan fault; XSHF, Xianshuihe fault; ANHF, Anninghe fault; ZMHF, Zemuhe fault; LD‐ZTF, Ludian–Zhaotong fault; XJF, Xiaojiang fault; HHF, Honghe fault; NTHF, Nantinghe fault; and LL‐LCJF, Longling–Lancangjiang fault. Seismic stations are shown in gray triangles, of which used in this study are marked
Journal Article
Journal: Interpretation
Published: 14 January 2019
Interpretation (2019) 7 (1): T195–T206.
...Naiquan Sun; Jie Pan; Sibin Zhou; Chunbo Jiao Abstract The Chang 8 (C8) reservoir is a transitional oil pool type from a tight oil sandstone to a lithologic trap in the Upper Triassic Yanchang Formation of the Honghe oil field, southwest Ordos Basin, China. Vertical faults play important roles...
FIGURES | View All (12)
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 06 December 2022
Lithosphere (2022) 2022 (Special 12): 9049312.
... dip-slip fault array. At the end of the late Miocene, the strike-slip activity of the Honghe-Yinggehai fault system in the western South China Sea [ 47 – 49 ] caused the tectonic uplift. It formed geomorphic units of platforms and slopes in this area. It leads to forming normal dip-slip faults...
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Image
Published: 10 May 2023
). The N-S–trending normal fault systems are according to Bian et al. (2021). SKS—South Kunlun suture; JHS—Jinsha-Honghe suture; BNS—Bangong-Nujiang suture; EHS—the east Himalayan syntaxis; SS—Shyok suture; UPV—ultrapotassic-potassic volcanic rocks; WHS—the west Himalayan syntaxis. (B) Diachronous
Image
Published: 01 April 2020
Figure 1. Simplified fault map of the Namche Barwa syntaxis that belongs to the eastern syntaxis (ES) of the Tibetan plateau. Thin red lines show active faults, while the thick red lines show strands of the Jiali fault (JLF). Blue lines represent river systems. The white triangle (JL‐01
Journal Article
Journal: Economic Geology
Published: 01 January 2003
Economic Geology (2003) 98 (1): 125–145.
... in eastern Tibet, which accommodated the compressive strains produced by the Asian-Indian continent collision, also localized the porphyry Cu mineralization. North to north-northeast–directed convergence and collision produced a dextral strike-slip fault system around 60 to 70 Ma. Northeast-directed wedging...
FIGURES | View All (11)
Journal Article
Published: 23 June 2020
Bulletin of the Seismological Society of America (2020) 110 (6): 3064–3076.
..., which led to stress accumulation and release causing earthquakes along the Honghe and Xiaojiang faults. The results from this study reveal a high‐velocity structure with a subducted slab‐like appearance that may represent vestiges of the Paleo‐Tethys oceanic lithosphere, which subducted beneath the ELIP...
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Journal Article
Published: 09 September 2022
Seismological Research Letters (2023) 94 (1): 189–205.
... occurred, concentrated in the depth of 6–15 km ( Qiang et al ., 2021 ). Qiaohou fault is located near the epicenter of the Yangbi earthquake, with a strike of north‐northwest and a length of about 280 km. It is connected with Honghe fault in the south and Jinshajiang fault in the north, connecting two...
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Journal Article
Journal: Interpretation
Published: 26 September 2022
Interpretation (2022) 10 (4): B25–B35.
... , Application of discontinuity attribute enhancement technology in fault controlled fracture detection of different scales in Shunbei area : Acta Geologica Sinica , 16 , 131 – 137 . AGSIDP Yang W. , 2009 , Sedimentary system and reservoir characteristics of Yanchang Formation in Zhenyuan...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 05 February 2022
Lithosphere (2021) 2021 (Special 7): 2541884.
... the Sanjiang orogenic system to the Yangtze platform and is also located in the NE trending fold area of the NW trending Honghe fault [ 16 ]. Its tectonic units are the South China fold belt (first-order) and the Southeast Yunnan fold belt (second-order). The regional seismotectonic is shown in Figure 2...
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Journal Article
Published: 01 December 1983
Bulletin of the Seismological Society of America (1983) 73 (6A): 1585–1597.
... (USGS)] occurred in Yunnan Province on the Qujiang fault, which is parallel to and possibly a branch of the much longer right-lateral Honghe (Red River) fault system. The 6 February 1973, Luhuo earthquake [Ms = 7.9 (China), 7.5 (USGS)] occurred in Sichuan Province on the left-lateral Xianshuihe fault...
Journal Article
Journal: GSA Bulletin
Published: 04 October 2024
GSA Bulletin (2025) 137 (3-4): 1315–1334.
...—Taiyuan Basin; LB—Linfen Basin; YB—Yuncheng Basin; WB—Weihe Basin; HB—Hetao Basin; YCB—Yinchuan Basin; F.—fault; S.—Shan. The extensional dynamics responsible for the formation of the Shanxi Rift system have been interpreted through three primary hypotheses: (1) the Indo-Asian collision prompted...
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Journal Article
Published: 01 April 2020
Seismological Research Letters (2020) 91 (3): 1776–1780.
...Figure 1. Simplified fault map of the Namche Barwa syntaxis that belongs to the eastern syntaxis (ES) of the Tibetan plateau. Thin red lines show active faults, while the thick red lines show strands of the Jiali fault (JLF). Blue lines represent river systems. The white triangle (JL‐01...
FIGURES | View All (4)
Journal Article
Published: 16 June 2022
Seismological Research Letters (2022) 93 (5): 2484–2497.
... not only delineates detailed geometry of the main fault system but also characterizes several branch faults, including two echelon subfaults crossing the north–south‐striking main fault. The velocity model shows strong lateral heterogeneities and exhibits a clear relationship to the seismicity distribution...
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Journal Article
Published: 10 November 2022
Bulletin of the Seismological Society of America (2023) 113 (1): 378–400.
... by the northeast‐oriented Lijiang–Xiaojinhe fault, and many large historical earthquakes (7.0 ≤ M ≤ 8.2) occurred along the surrounding deep and major faults, such as the Xianshuihe, Anninghe, Zemuhe, Xiaojiang, and Honghe faults. Considering the seismic safety demand for the large, exposed population...
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Journal Article
Published: 09 January 2018
Bulletin of the Seismological Society of America (2018) 108 (1): 101–115.
...Figure 1. Fault distributions around the Xichang fault bend, which has an angle of about 30°. Thick and thin lines denote active and inactive faults, respectively. The inset map shows the fault systems of the Tibetan plateau (modified after Tapponnier et al. , 2001 ). The base map is from...
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Journal Article
Published: 01 March 2013
Jour. Geol. Soc. India (2013) 81 (3): 415–421.
... fault zone and its tectonic evolution significance . Science in China Series D: Earth Sciences , v. 49 (8) , pp. 839 – 850 . Liu , H.L. , Yan , P. , Zhang , B.Y. , et al . (2004) Role of the Wan-Na fault system in the western Nansha Islands (Southern South China Sea) . Jour...
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