Volume 22 Issue 3
Sep.  2016
Turn off MathJax
Article Contents
CHANG Zu-feng, CHANG Hao, ZANG Yang, et al., 2016. RECENT ACTIVE FEATURES OF WEIXI-QIAOHOU FAULT AND ITS RELATIONSHIP WITH THE HONGHE FAULT. Journal of Geomechanics, 22 (3): 517-530.
Citation: CHANG Zu-feng, CHANG Hao, ZANG Yang, et al., 2016. RECENT ACTIVE FEATURES OF WEIXI-QIAOHOU FAULT AND ITS RELATIONSHIP WITH THE HONGHE FAULT. Journal of Geomechanics, 22 (3): 517-530.

RECENT ACTIVE FEATURES OF WEIXI-QIAOHOU FAULT AND ITS RELATIONSHIP WITH THE HONGHE FAULT

More Information
  • Received: 2016-04-09
  • Published: 2016-09-01
  • According to geological and geomorphic field observations, in this paper, we mainly elaborate the late Quaternary active features of the Weixi-Qiaohou fault, and discuss its relationship with the Honghe fault. The fault have apparently dominated many late Cenozoic basins' development, showing dextral strike slip motion features as being documented by synchronous right-lateral dislocation of mountain ridges and rivers along it. It has displaced late Pleistocene to Holocene accumulations revealed by the exploratory trenches at Desheng and the site south of Changyi. Nearby Yanqu and Shiyan, there is a 3 km long, ~2.5 m high fault scarp on the river terraces and the alluvial fans. It is estimated the fault has a average rate of 1.8~2.4 mm/yr. horizontally and 0.3~0.35 mm/yr. vertically since late Pleistocene, based on displaced magnitude of the alluvial fans, gullies and river terraces. It is a significant link which connects with the Honghe fault in the south and with the Jingshajiang fault in the north. Since late Cenozoic, the Weixi-Qiaohou fault in kinematics is similar to the Honghe fault and the Jinshajiang fault, they having identical geological evolutionary history and tectonic deformation mechanism, accordingly, indicating that the Weixi-Qiaohou fault should be the northern segment of the Honghe fault. The Weixi-Qiaohou, Honghe, Jinshajiang as well as Deqin-Zhongdian fault composed of the western boundary of Sichuan-Yunnan active block all together.

     

  • loading
  • [1]
    李玶, 汪良谋.云南川西地区地震地质基本特征的探讨[J].地质科学, 1975, 10(4):308~326. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX197504001.htm

    LI Ping, Wang Liang-mou. Discuss on the basic characteristics of seismotectonics inYunnan-Sichuan region[J].Chinese Journal of Geology, 1975, 10(4):308~326. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX197504001.htm
    [2]
    阚荣举, 张四昌, 晏凤桐.我国西南地区现代构造应力场与现代构造活动特征的探讨[J].地球物理学报, 1977, 20(2):96~109. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX197702001.htm

    KAN Rong-ju, ZHANG Si-chuang, YAN Feng-tong.1977. Discuss on modern tectonic stress field and the tectonic activity features in southern region, China[J]. Chinese Journal of Geophysics, 1977, 20(2):96~109. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX197702001.htm
    [3]
    邓起东, 张培震, 冉勇康, 等.中国活动构造基本特征[J].中国科学(D辑), 2002, 32(12):1020~1030. doi: 10.3321/j.issn:1006-9267.2002.12.007

    DENG Qidong, ZHANG Peizhen, RAN Yongkang, et al. Basic characteristics of active tectonics in China[J]. Science in China (Series D), 2002, 32(12):1020~1030. doi: 10.3321/j.issn:1006-9267.2002.12.007
    [4]
    徐锡伟, 闻学泽, 郑荣章, 等.川滇地区活动块体最新构造样式及动力学来源[J].中国科学(D辑), 2003, 33(增刊):151~162.

    XU Xi-wei, WEN Xue-ze, ZHENG Rong-zhang, et al. Pattern of latest tectonic motion and dynamics of faulted blocks in Yunnan and Sichuan[J]. Science in China (Series D), 2003, 33(Suppl):151~162.
    [5]
    张家声, 李燕, 韩竹均.青藏高原向东挤出的变形响应及南北地震带构造组成[J].地学前缘, 2003, 10(特刊):168~175. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1023.htm

    ZHANG Jia-sheng, LI Yan, HAN Zhu-jun. Deformation responses to eastwards escaping of the Qinghai Tibet plateau and tectonics of the South-North seismic zone in China[J]. Earth Science Frontiers, 2003, 10(suppl):168~175. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1023.htm
    [6]
    张培震, 王敏, 甘卫军, 等. GPS观测的活动断裂滑动速率及其对现今大陆动力作用的制约[J].地学前缘, 2003a, 10(增刊):81~92. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1013.htm

    ZHANG Pei-Zhen, WANG Min, GAN Wei-jun, et al.Slip rates along major active faults from GPS measurements and constrains on contemporary continental tectonics[J].Earth Science Frontiers, 2003a, 10(Suppl):81~92. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1013.htm
    [7]
    张培震, 邓起东, 张国民, 等.中国大陆的强震活动与活动地块[J].中国科学(D辑), 2003b, 33(增刊):12~20. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1012.htm

    ZHANG Pei-zhen, DENG Qi-dong, ZHANG Guo-min, et al..Active tectonic blocks and strong earthquakes in continental China[J]. Science in China(Series D), 2003b, 33(Suppl):12~20. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1012.htm
    [8]
    吕江宁, 沈正康, 王敏.川滇地区现代地壳运动速度场和活动块体模型研究[J].地震地质, 2003, 25(4):543~554. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200304002.htm

    LU Jiang-ning, SHEN Zheng-kang, WANG Min.Velocity field and tectonic block division of crustal movement obtained by GPS measurements in Sichuan-Yunnan region[J]. Seismology and Geology, 2003, 25(4):543~554. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200304002.htm
    [9]
    SHEN Z K, LU J N, WANG M, et al. Contemporary crustal deformation around the southeast borderland of the Tibetan Plateau[J]. Journal Geophysical Research, 2005, 110:B11409.
    [10]
    WANG Q, ZHANG P Z., FREYMUELLER J T, et al. Present-day crustal deformation in China constrained by Global Positioning System measurements[J].Science, 2001, 294:574~577. doi: 10.1126/science.1063647
    [11]
    ZHANG P Z, SHEN Z.K, WANG M, et al. Continuous deformation of the Tibetan Plateau from global positioning system data[J]. Geology, 2004, 32:809~812. doi: 10.1130/G20554.1
    [12]
    王阎昭, 王恩宁, 沈正康, 等.基于GPS资料约束反演川滇地区主要断裂现今活动速率[J].中国科学(D辑):地球科学, 2008, 38(5):582~597. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200805006.htm

    WANG Yan-zhao, WANG En-ning, SHEN Zheng-kang, et al.GPS-constrained inversion of present-day slip rates along major faults of the Sichuan-Yunnan region, China[J].Science in China (Series D):Earth Sciences, 2008, 51(9):582~597. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200805006.htm
    [13]
    ALLEN C R, LUO Z, QIAN H, et al. Field study of a highly active fault zone:The Xianshuihe fault of southern China[J]. Geological Society of America Bulletin, 1989, 103:1178~1199. doi: 10.1007/s11589-008-0009-7
    [14]
    闻学泽.鲜水河断裂带未来三十年地震复发的条件概率[J].中国地震, 1990, 6(4):8~16. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD199004001.htm

    WEN Xue-ze. The earthquake recurrence condition probability in next 30 years along Xianshuihe faults[J].Earthquake research in China, 1990, 6(4):8~16. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD199004001.htm
    [15]
    郭晓虎, 魏东平, 张克亮.GPS约束下川滇地区主要断裂现今活动速率的估算方法[J].中国科学院研究生院学报, 2013, 30(1):74~82. http://www.cnki.com.cn/Article/CJFDTOTAL-ZKYB201301013.htm

    GUO Xiao-hu, WEI Dong-ping, ZHANG Ke-liang. GPS-constrained estimate method of present-day slip rate along major faults of Sichuan-Yunnan region in China. Journal of Graduate University of Chinese Academy of Sciences, 2013, 30(1):74~82. http://www.cnki.com.cn/Article/CJFDTOTAL-ZKYB201301013.htm
    [16]
    潘懋, 梁海华, 蔡永恩, 等.中国川西地区鲜水河断裂和则木河断裂几何学、运动学特征及地震活动性对比研究[J].中国地震, 1994, 10(1):28~37. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD401.004.htm

    PAN Mao, LIANG Haihua, CAI Yongen, et al. Comparision between the Xianshuihe fault zone and Zemuhe fult zone[J]. Earthquake research in China, 1994, 10(1):28~37. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD401.004.htm
    [17]
    冉勇康, 陈立春, 程建武, 等.安宁河断裂冕宁以北晚第四纪地表变形与强震破裂行为[J].中国科学(D辑), 2008, 38(5):543~554. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200805002.htm

    RAN Yong-kang, CHEN Li-chun, CHENG Jian-wu, et a l.2008.Late Quaternary surface deformation and rupture behavior of strong earthquake on the segment north of Mianning of the Anninghe Fault[J].Science in China(Series D), 38(5):543~554. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200805002.htm
    [18]
    李玶.鲜水河-小江断裂带[M].北京:地震出版社, 1993.

    LI Ping. The Xianshuihe-Xiaojiang fault zone[M]. Earthquake Press, Beijing, 1993.
    [19]
    唐文清, 刘宇平, 陈智梁, 等.鲜水河断裂及两侧地块的GPS监测[J].西南交通大学学报, 2005, 40(3):13~317. http://www.cnki.com.cn/Article/CJFDTOTAL-XNJT200503005.htm

    TANG Wen-qing, LIU Yu-ping, CHEN Zhi-liang, et al.GPS monitoring of Xianshuihe fault and blocks on Its both sides[J].Journal of Southwest Jiaotong University, 2005, 40(3):13~317. http://www.cnki.com.cn/Article/CJFDTOTAL-XNJT200503005.htm
    [20]
    熊探宇, 姚鑫, 张永双.鲜水河断裂带全新世活动性研究进展综述[J].地质力学学报, 2010, 16(2):176~188. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100206&flag=1

    XIONG Tan-yu, YAO Xin, ZHANG Yong-shuang. A review on study of activity of Xianshuihe fault zone since the Holocene[J].Journal of Geomechanics, 2010, 16(2):176~188. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100206&flag=1
    [21]
    TAPPONNIER P, ZHIQIN X, ROGER F, et al. Oblique stepwise rise and growth of Tibet plateau[J].Science, 2001, 294, No.5547, 1671~1677. doi: 10.1126/science.105978
    [22]
    TAPPONNIER P, PELTZER G, DAIN A Le, et al. Propogation extrution tectonics in Aisa:New insights from simple experiments with plasticine[J].Geology, 1982, 10:61~616. doi: 10.1130/0091-7613(1982)10<61a:CAROIO>2.0.CO;2
    [23]
    TAPPONNIER P, PELTZER G, ARMIJO R. On the mechanics of the collision between India and Asia, in Coward, M. P., and Ries, A. C., eds., Collision Tectonics[M].Geological Society London Special Publication, 1986, 19:115~157.
    [24]
    TAPPONNIER P, LACASSIN R, LELOUP P H, et al. The Ailao shan/Red River metamorphic belt:Tertiary left-lateral shear between Indochina and south China[J]. Nature, 1990, 343:431~437. doi: 10.1038/343431a0
    [25]
    LELOUP P H, KIENAST J R. High temperature metamorphism in a major strike-slip shear zone:the Ailao Shan-Red River (P.R.C)[J]. Earth Planetary Science Letters, 1993, 188:213~234. doi: 10.1007/978-3-319-25235-3_8
    [26]
    LELOUP P H, LACASSIN R, TAPPONNIER P, et al. The Ailao Shan-Red River shear zone (Yunnan China), Tertiary transform boundary of Indochina[J]. Tectonophysics, 1995, 251:3~84. doi: 10.1016/0040-1951(95)00070-4
    [27]
    SCHOENBOHM L M, BURCHFIEL B C, CHEN L, et al. Miocene to present activity along the Red River fault, China, in the context of continental extrusion, upper-crustal rotation, and lower-crustal flow[J]. Geological Society of America Bulletin, 2006, 118(5/6):672~688.
    [28]
    SOCQUET A, PUBELLIER M. Cenozoic deformation in western Yunnan (China-Myanmar border)[J]. Journal of Asian Earth Science, 2005, 24:495~515. doi: 10.1016/j.jseaes.2004.03.006
    [29]
    陈文寄, 李齐, 汪一鹏.哀牢山-红河左旋走滑剪切带中新世抬升的时间序列[J].地质论评, 1996, 42(5):385~390. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199605000.htm

    CHEN Wen-ji, LI Qi, WANG Yi-peng. Miocene diachronic uplift Ailao mountains-Red River left lateral strike-slip shear zone[J]. Geological Review, 1996, 42(5):385~390. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199605000.htm
    [30]
    虢顺民, 计凤洁, 向宏发, 等.红河活动断裂带[M].北京:海洋出版社, 2001.

    GUO Shun-min, Ji Feng-ju, XIANG Hong-fa, et al. The Honghe active fault zone[M]. Marine Press, Beijing, 2001.
    [31]
    向宏发, 虢顺民, 张晚霞, 等.红河断裂带南段中新世以来大型右旋位错量的定量研究[J].地震地质, 2007, 29(1):52~65. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200701002.htm

    XIANG Hong-fa, GUO Shun-min, Zhang Wan-xia, et al. Quantitative study on the large scale dextral strike slip offset in the southern segment of the Red River Fault since Miocene[J]. seismology and geology, 2007, 29(1):52~65. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200701002.htm
    [32]
    向宏发, 韩竹军, 虢顺民, 等.红河断裂带大型右旋走滑运动与伴生构造地貌变形[J].地震地质, 2004, 26(4):43~56. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200404005.htm

    XIANG Hong-fa, HAN Zhu-jun, GUO Shun-min, et al. Large-scale dextral strike-slip movement and associated tectonic deformation along the red-river fault zone[J].Seismology and geology, 2004, 26(4):43~56. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200404005.htm
    [32]
    王绍晋, 张建国, 余庆坤, 等.红河断裂带的震源机制与现代构造应力场[J].地震研究, 2010, 33(2):200~207. http://www.cnki.com.cn/Article/CJFDTOTAL-DZYJ201002015.htm

    WANG Shao-jin, ZHANG Jian-guo, YU Qing-kun, et al. Focal Mechanism of Strong and Medium small Earthquakes and Modern Tectonic Stress Field of the Red River Fault Zone[J].Journal of seismological research, 2010, 33(2):200~207. http://www.cnki.com.cn/Article/CJFDTOTAL-DZYJ201002015.htm
    [33]
    乔学军, 王琪, 杜瑞林.川滇地区活动地块现今地壳形变特征[J].地球物理学报, 2004, (5):805~811. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200405010.htm

    QIAO Xue-jun, WANG Qi, DU Rui-lin. Characteristics of current crustal deformation of active blocks in the sichuan-yunnan region[J]. Chinese Journal of Geophysics, 2004, (5):805~811. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200405010.htm
    [34]
    WANG E, BURCHFIEL B C, ROYDEN L H, et al. Late Cenozoic Xianshuihe-Xiaojiang, Red River, and Dali fault systems of southwestern Sichuan and central Yunnan, China[J]. Special Paper of the Geological Society of American, 1998, 327:1~108. http://www.worldcat.org/title/late-cenozoic-xianshuihe-xiaojiang-red-river-and-dali-fault-systems-of-southwestern-sichuan-and-central-yunnan-china/oclc/488828647
    [35]
    ALLEN C R, GILLESPIE A R, HAN Y, et al. Red River and associated faults, Yunnan province, China:Quaternary geology, slip rate and Seismic hazard[J]. Geological Society of America Bulletin, 1984, 95:686~700. doi: 10.1130/0016-7606(1984)95<686:RRAAFY>2.0.CO;2
    [36]
    许志琴, 侯立玮, 王综秀, 等.中国松潘-甘孜造山带的造山过程[M].北京:地质出版社, 1992.

    XU Zhi-qin, HOU Li-wei, WANG Zong-xiu. et al. The Songpan Ganzi Orogeny process in China[M]. Geological Publishing House, Beijing, 1992.
    [37]
    唐荣昌, 韩渭滨.四川活动断裂与地震[M].北京:地震出版社, 1993.

    TANG Rong-chang, HAN Wei-bin. Active faults and earthquakes in Sichuan[M]. Seismology Press, Beijing, 1993.
    [38]
    常祖峰, 2013年云南奔子栏M5.9级地震发生的地震地质背景, 地震地质, 2015, 37(1):192~207. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201501015.htm

    CHANG Zu-feng, The seismotectonic background of the 2013 Benzilan M5.9 earthquake, Yunan Province[J].Seismology and geology, 2015, 37(1):192~207. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201501015.htm
    [39]
    汪一鹏, 沈军, 王琪, 等.川滇块体的侧向挤出问题[J].2003, 地学前缘, 10(特刊):187~192. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1025.htm

    WANG Yi-peng, SHEN Jun, WANG Qi, et al. On The Lateral Extrusion Ofs Ichuan-Yunnan Block (Chuandian Block)[J]. Earth Science Frontiers, 2003, 10(Suppl.):187~192. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY2003S1025.htm
    [40]
    马宗晋, 张家声, 汪一鹏. 青藏高原三维变形运动随时间的变化[A]. 见: 现代地壳运动与地球动力学研究[M]. 北京: 地震出版社, 2001.

    MA Zong-jin, ZHANG Jia-sheng, WANG Yi-peng. The 3-D deformation movement episodes of the Qinghai-Xizang plateau[A]. In:Study on the recent deformation and dynamics of the Lithosphere of Qinghai-Xizang plateau[M]. Seismology Press, Beijing, 2001.
    [41]
    钟大赉, 丁林.青藏高原的隆起过程及其机制探讨[J].中国科学(D辑), 1996, 26(4):289~295. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199604000.htm

    ZHONG Da-lai, DING Lin.1996. Rising process of the Qinghai-Xizang(Tibet) Plateau and its mechanism[J].Science in China(Series D), 26(4):289-295. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199604000.htm
    [42]
    TAPPONNIER P, MOLNAR P. Active faulting and tectonics of China[J]. Journal Geophysical Research, 1977, 82(20):2905~2930. doi: 10.1029/JB082i020p02905
    [43]
    MOLNAR P, TAPPONNIER P. Cenozoic tectonics of Asia:effects of a continental collision[J]. Science, 1975, 189:419~426. doi: 10.1126/science.189.4201.419
    [44]
    PELTZER G, TAPPONNIER P. Formation and evolution of strike-slip faults, rifts, and basins during India-Asia collision:an experiment approach[J]. Journal Geophysical Research, 1988, 93:15085~15117. doi: 10.1029/JB093iB12p15085
    [45]
    ARMIJO R P, TAPPONNIER J, MERCIER, et al. Late Cenozoic right-lateral strike-slip faulting in southern Tibet[J]. Journal Geophysical Research1989, 94, No.B3, 2787~2838. doi: 10.1029/JB094iB03p02787
    [46]
    云南省地质矿产局. 云南省区域地质志[M]. 北京: 地质出版社, 1990.

    Bureau of Geology and Mineral Resources of Yunnan Province. Regional geology of Yunnan Province[M]. Geological Publishing House, Beijing, 1990.
    [47]
    常祖峰, 张艳凤, 李鉴林, 等.德钦-中甸-大具断裂晚第四纪活动的地质与地貌表现[J].地震研究, 2014, 37(1):46~52. http://www.cnki.com.cn/Article/CJFDTOTAL-DZYJ201401007.htm

    CHANG Zu-feng, ZHANG Yan-feng, LI Jian-lin, et al. The geological and geomorphic characteristic of late Quaternary activity of the Deqin-Zhongdian-Daju fault[J].Journal of Seismological Research, 2014, 37(1):46~52. http://www.cnki.com.cn/Article/CJFDTOTAL-DZYJ201401007.htm
  • 加载中

Catalog

    Figures(12)

    Article Metrics

    Article views (267) PDF downloads(62) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return