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HUANG Xiaolong, WU Zhonghai, WU Kungang. 2021. Late Cenozoic development characteristics and dynamic mechanism of the main faults in the Midu area, northwestern Yunnan[BP(]Development characteristics of the main faults of the late cenozoic in the Midu area, northwestern Yunnan, and their dynamic mechanism. Journal of Geomechanics, 27(6): 913-927. doi: 10.12090/j.issn.1006-6616.2021.27.06.074
Citation: HUANG Xiaolong, WU Zhonghai, WU Kungang. 2021. Late Cenozoic development characteristics and dynamic mechanism of the main faults in the Midu area, northwestern Yunnan[BP(]Development characteristics of the main faults of the late cenozoic in the Midu area, northwestern Yunnan, and their dynamic mechanism. Journal of Geomechanics, 27(6): 913-927. doi: 10.12090/j.issn.1006-6616.2021.27.06.074
shu

Late Cenozoic development characteristics and dynamic mechanism of the main faults in the Midu area, northwestern Yunnan[BP(]Development characteristics of the main faults of the late cenozoic in the Midu area, northwestern Yunnan, and their dynamic mechanism

  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    Key Laboratory of Neotectonic Movement and Geohazard, Institute of Geomechanics, Beijing 100081, China

  • 3.

    Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China

  • 4.

    China University of Geosciences, Beijing 100083, China

    • Fund Project: This research is financially supported by the National Natural Science Foundation of China (Grant No.41571013, U2002211), the China Geological Survey Project (Grant No.DD20160268, 12120114002101) and the Basic Research Funds of Institute of Geomechanics, Chinese Academy of Geological Sciences (Grant No.DZLXJK201702)
More Information
Received Date:  09 April 2021
Revised Date:  20 August 2021
Publish Date:  28 December 2021
    Abstract

  • The Midu area is located at the southeast end of the northwestern Yunnan fault depression zone, the intersection of the Red River fault zone and the Chenghai fault. It is a key area for uncovering the formation mechanism of the Northwest Yunnan fault depression zone as well as its kinematic relationship with the Red River fault zone. Based on remote sensing interpretation and field investigation, we found five faults in the study area, namely the NE-trending Maolipo fault, NW-NNW-trending Fengyi-Dingxiling fault, Midu fault, Mizhi fault and Yinjie fault. We made statistical analysis of the fault slipping geological-landscape bodies and slickensides, and the results are produced in three aspects. Firstly, the Maolipo fault are mainly characterized by left lateral strike-slip activity with normal fault component in Quaternary. Secondly, the arc-shaped Midu fault and the NW-trending Yinjie fault are dominated by normal fault activity in Quaternary. Thirdly, during the Pliocene the Fengyi-Dingxiling fault was characterized by dextral strike-slips, while the Mizhi fault by extensional normal faults, and there was no obvious activity in both faults during the Quaternary. We inferred both from the geometry and kinematics of the main faults in the Midu area and the activity evolution of the Red River fault zone that, in the Late Cenozoic the main Quaternary active faults, such as the Midu fault and Yinjie fault, were formed on the basis of inheriting and remaking the original fault trace of the Red River fault zone. These active faults controlled the distribution of the Midu basin. The fault activity and transtensional deformation in the Midu area and the Northwest Yunnan fault depression zone during the Pliocene or even earlier could be affected by the extensional deformation at the end of the Red River fault zone. However, during the Quaternary the Chenghai fault basically controlled the development of main active faults in the Midu area. The crustal transtensional deformation in this period might be driven by the clockwise rotation of the Sichuan-Yunnan inner arc belt and the regional strike-slip pull-apart caused by the Nantinghe fault, Wanding fault and Litang fault.

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    • References
  • ALLEN C R, GILLESPIE A R, YUAN H, et al., 1984. Red River and associated faults, Yunnan Province, China: Quaternary geology, slip rates, and seismic hazard[J]. GSA Bulletin, 95(6): 686-700. doi: 10.1130/0016-7606(1984)95<686:RRAAFY>2.0.CO;2

    CrossRef Google Scholar

    ALLEN C R, LUO Z L, QIAN H, et al., 1991. Field study of a highly active fault zone: The Xianshuihe fault of southwestern China[J]. Geological Society of America Bulletin, 103(9): 1178-1199. doi: 10.1130/0016-7606(1991)103<1178:FSOAHA>2.3.CO;2

    CrossRef Google Scholar

    Bureau of Geology and Mineral Resources of Yunnan Province, 1990. Regional geology of Yunnan province[M]. Beijing: China Geological Press: 1-728. (in Chinese)

    Google Scholar

    CHANG Z F, CHANG H, ZANG Y et al., 2016. Recent active features of Weixi-Qiaohou fault and its relationship with the Honghe fault[J]. Journal of Geomechanics, 22(3): 517-530. (in Chinese with English abstract)

    Google Scholar

    CHEN W J, LI Q, WANG Y P, 1996. Miocene diachronic uplift along the Ailao Mountains Red river left-lateral strike-slip shear zone[J]. Geological Review, 42(5): 385-390. (in Chinese with English abstract)

    Google Scholar

    CHEN Z, BURCHFIEL B C, LIU Y, et al., 2000. Global Positioning System measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation[J]. Journal of Geophysical Research: Solid Earth, 105(B7): 16215-16227. doi: 10.1029/2000JB900092

    CrossRef Google Scholar

    CUI X F, XIE F R, ZHANG H Y, 2006. Recent tectonic stress field zoning in Sichuan-Yunnan region and its dynamic interest[J]. Acta Seismologica Sinica, 19(5): 485-496. doi: 10.1007/s11589-006-0501-x

    CrossRef Google Scholar

    FAN C, WANG G, WANG S F, et al., 2006. Structural interpretation of extensional deformation along the Dali fault system, southeastern margin of the Tibetan Plateau[J]. International Geology Review, 48(4): 287-310. doi: 10.2747/0020-6814.48.4.287

    CrossRef Google Scholar

    GUO S M, XIANG H F, JI F J, et al., 1996. A study on the relation between Quaternary right-lateral slip and tip extension along the Honghe fault[J]. Seismology and Geology, 18(4): 301-309. (in Chinese with English abstract)

    Google Scholar

    GUO S M, JI F J, XIANG H F, et al., 2001. The Honghe active fault zone[M]. Beijing: China Ocean Press: 1-172. (in Chinese)

    Google Scholar

    HAN Z J, XIANG H F, GUO S M, 2005. Sinistral shear and extension of the northern section of Lijiang Basin in northwest Yunnan in quaternary[J]. Chinese Science Bulletin, 50(5): 452-459. doi: 10.1007/BF02897462

    CrossRef Google Scholar

    HARRISON T M, CHEN W J, LELOUP P H, et al., 1992. An early Miocene Transition in deformation regime within the Red River Fault Zone, Yunnan, And its significance for Indo-Asian tectonics[J]. Journal of Geophysical Research: Solid Earth, 97(B5): 7159-7182. doi: 10.1029/92JB00109

    CrossRef Google Scholar

    HUANG X J, WU Z H, LI J C, et al., 2014. Tectonic geomorphology and Quaternary tectonic activity in the northwest Yunnan rift zone[J]. Geological Bulletin of China, 33(4): 578-593. (in Chinese with English abstract)

    Google Scholar

    HUANG X L, WU Z H, WU K G, et al., 2016. The main active faults and tectonic system in Yongsheng area, northwest Yunnan[J]. Journal of Geomechanics, 22(3): 531-547. (in Chinese with English abstract)

    Google Scholar

    HUANG X J, WU Z H, HUANG X L, et al., 2018. Tectonic geomorphology constrains on Quaternary activity and segmentation along Chenghai-Binchuan fault zone in northwest Yunnan, China[J]. Earth Science, 43(12): 4651-4670. (in Chinese with English abstract)

    Google Scholar

    HUANG X L, WU Z H, WU K G, 2018. Surface rupture of the 1515 Yongsheng earthquake in Northwest Yunnan, and its seismogeological implications[J]. Acta Geologica Sinica (English Edition), 92(4): 1324-1333. doi: 10.1111/1755-6724.13629

    CrossRef Google Scholar

    HUANG X L, WU Z H, LIU F, et al., 2021. Tectonic interpretation of the main paleoseismic landslides and their distribution characteristics in the Chenghai fault zone, Northwest Yunnan[J]. Earth Science Frontiers, 28(2): 125-139. (in Chinese with English abstract)

    Google Scholar

    , 1990. Active faults in Northwest Yunnan[M]. Beijing: Seismological Press: 1-321. (in Chinese)

    Google Scholar

    Jian Zi 730 unit of the Chinese people's Liberation Army. 1978. 1: 200000 Dali hydrogeological survey results report[Z]. (in Chinese)

    Google Scholar

    LACASSIN R, SCHÄRER U, LELOUP P H, et al., 1996. Tertiary deformation and metamorphism SE of Tibet: The folded Tiger-leap décollement of NW Yunnan, China[J]. Tectonics, 15(3): 605-622. doi: 10.1029/95TC03749

    CrossRef Google Scholar

    LELOUP P H, HARRISON T M, RYERSON F J, et al., 1993. Structural, petrological and thermal evolution of a Tertiary ductile strike-slip shear zone, Diancang Shan, Yunnan[J]. Journal of Geophysical Research: Solid Earth, 98(B4): 6715-6743. doi: 10.1029/92JB02791

    CrossRef Google Scholar

    LELOUP P H, LACASSIN R, TAPPONNIER P, et al., 1995. The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina[J]. Tectonophysics, 251(1-4): 3-84. doi: 10.1016/0040-1951(95)00070-4

    CrossRef Google Scholar

    LI G R, JIN D S, 1990. Neoid activity on the Chenghai fracture[J]. Yunnan Geology, 9(1): 1-24. (in Chinese with English abstract)

    Google Scholar

    LI P, WANG L M, 1975. Exploration of the seismo-geological features of the Yunnan-West Sichuan region[J]. Scientia Geologica Sinica, 10(4): 308-326. (in Chinese with English abstract)

    Google Scholar

    LIU G X, LI F Q, LI G R, 1986. Active tectonics and state of stress in seismic region of north-west Yunnan province, China[J]. Seismology and Geology, 8(1): 1-14. (in Chinese with English abstract)

    Google Scholar

    LUO R J, WU Z H, HUANG X L, et al., 2015. The main active faults and the active tectonic system of Binchuan area, northwestern Yunnan[J]. Geological Bulletin of China, 34(1): 155-170. (in Chinese with English abstract)

    Google Scholar

    PAN G T, XIAO Q H, LU S N, et al., 2009. Subdivision of tectonic units in China[J]. Geology in China, 36(1): 1-28. (in Chinese with English abstract)

    Google Scholar

    QIAN X D, SU Y J, FU H, et al., 2011. Short-term and Impending Prediction of the Mar. 10, 2011, MS5.8, Yingjiang, Yunnan Earthquake[J]. Journal of seismological research, 34(4): 403-413. (in Chinese with English abstract)

    Google Scholar

    SCHOENBOHM L M, WHIPPLE K X, BURCHFIEL B C, et al., 2004. Geomorphic constraints on surface uplift, exhumation, and plateau growth in the Red River region, Yunnan Province, China[J]. GSA Bulletin, 116(7-8): 895-909.

    Google Scholar

    SCHOENBOHM L M, BURCHFIEL B C, CHEN L Z, et al., 2006. Miocene to present activity along the Red River fault, China, in the context of continental extrusion, upper-crustal rotation, and lower-crustal flow[J]. GSA Bulletin, 118(5-6): 672-688. doi: 10.1130/B25816.1

    CrossRef Google Scholar

    SHEN Z K, LÜ J N, WANG M, et al., 2005. Contemporary crustal deformation around the southeast borderland of the Tibetan Plateau[J]. Journal of Geophysical Research: Solid Earth, 110(B11): B11409.

    Google Scholar

    SHI X H, WANG Y, SIEH K, et al., 2018. Fault slip and GPS velocities across the Shan Plateau define a curved southwestward crustal motion around the eastern Himalayan syntaxis[J]. Journal of Geophysical Research: Solid Earth, 123(3): 2502-2518. doi: 10.1002/2017JB015206

    CrossRef Google Scholar

    SOCQUET A, PUBELLIER M, 2005. Cenozoic deformation in western Yunnan (China-Myanmar border)[J]. Journal of Asian Earth Sciences, 24(4): 495-515. doi: 10.1016/j.jseaes.2004.03.006

    CrossRef Google Scholar

    TAPPONNIER P, MOLNAR P, 1976. Slip-line field theory and large-scale continental tectonics[J]. Nature, 264(5584): 319-324. doi: 10.1038/264319a0

    CrossRef Google Scholar

    TAPPONNIER P, PELTZER G, LE DAIN A Y, et al., 1982. Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine[J]. Geology, 10(12): 611-616. doi: 10.1130/0091-7613(1982)10<611:PETIAN>2.0.CO;2

    CrossRef Google Scholar

    TAPPONNIER P, PELTZER G, ARMIJO R, 1986. On the mechanics of the collision between India and Asia[J]. Geological Society, London, Special Publications, 19(1): 113-157. doi: 10.1144/GSL.SP.1986.019.01.07

    CrossRef Google Scholar

    TAPPONNIER P, LACASSIN R, LELOUP P H, et al., 1990. The Ailao Shan/Red River metamorphic belt: Tertiary left-lateral shear between Indochina and South China[J]. Nature, 343(6257): 431-437. doi: 10.1038/343431a0

    CrossRef Google Scholar

    TAPPONNIER P, XU Z Q, ROGER F, et al., 2001. Oblique stepwise rise and growth of the Tibet plateau[J]. Science, 294(5547): 1671-1677. doi: 10.1126/science.105978

    CrossRef Google Scholar

    WANG E C E, BURCHFIEL B C, 1997. Interpretation of cenozoic tectonics in the right-lateral accommodation zone between the Ailao Shan Shear zone and the eastern Himalayan Syntaxis[J]. International Geology Review, 39(3): 191-219. doi: 10.1080/00206819709465267

    CrossRef Google Scholar

    WANG E, BURCHFIEL B C, ROYDEN L H, et al., 1998. Late Cenozoic Xianshuihe-Xiaojiang, Red River, and Dali fault systems of southwestern Sichuan and central Yunnan, China[M]. Boulder: Geological Society of America, 327: 1-108.

    Google Scholar

    WU D N, DENG Q D, 1985. The basic taphrogenic feature in Northwestern Yunnan and its formation mechanism[M]//Institute of Geology, State Seismological Administration, ed. Research on Recent Crustal Movement (1): Continental Rifting and Deep Processes. Beijing: Seismological Press: 118-132. (in Chinese)

    Google Scholar

    WU Z H, ZHANG Y S, HU D G, et al., 2009. Late Quaternary normal faulting and its kinematic mechanism of eastern piedmont fault of the Haba-Yulong Snow Mountains in northwestern Yunnan, China[J]. Science in China Series D: Earth Sciences, 52(10): 1470-1484. doi: 10.1007/s11430-009-0148-2

    CrossRef Google Scholar

    WU Z H, LONG C X, FAN T Y, et al., 2015. The arc rotational-shear active tectonic system on the southeastern margin of Tibetan Plateau and its dynamic characteristics and mechanism[J]. Geological Bulletin of China, 34(1): 1-31. (in Chinese with English abstract)

    Google Scholar

    XIANG H F, GUO S M, RANG Y K, et al., 1986. Recent tectonic stress field in the northwest of the Yunnan province[J]. Seismology and Geology, 8(1): 15-23. (in Chinese with English abstract)

    Google Scholar

    XIANG H F, GUO S M, XU X W, et al., 2000. Active block division and present-day motion features of the south region of Sichuan-Yunnan province[J]. Seismology and Geology, 22(3): 253-264. (in Chinese with English abstract)

    Google Scholar

    XIAO K Z, TONG H M. 2020. Progress on strike-slip fault research and its significance[J]. Journal of Geomechanics, 26(2): 151-166. (in Chinese with English abstract)

    Google Scholar

    XU X W, GUO S M, ZHENG R Z, et al., 2003. Pattern of latest tectonic motion and its dynamics for active blocks in Sichuan-Yunnan region, China[J]. Science in China Series D: Earth Sciences, 46(2): 210-226.

    Google Scholar

    ZHANG J G, HUANG F G, XIE Y Q, et al., 2009. Study on the activity of Red river fault in Vietnam[J]. Seismology and geology, 31(3): 389-400. (in Chinese with English abstract)

    Google Scholar

    ZHANG P Z, SHEN Z K, WANG M, et al., 2004. Continuous deformation of the Tibetan Plateau from global positioning system data[J]. Geology, 32(9): 809-812. doi: 10.1130/G20554.1

    CrossRef Google Scholar

    ZHANG Y Z, REPLUMAZ A, WANG G C, et al., 2015. Timing and rate of exhumation along the Litang fault system, implication for fault reorganization in South East Tibet[J]. Tectonics, 34(6): 1219-1243. doi: 10.1002/2014TC003671

    CrossRef Google Scholar

    ZHENG W J, ZHANG P Z, YUAN D Y, et al., 2019. Basic characteristics of active tectonics and associated geodynamic processes in continental china[J]. Journal of Geomechanics, 25(5): 699-721. (in Chinese with English abstract)

    Google Scholar

    常祖峰, 常昊, 臧阳, 等, 2016. 维西-乔后断裂新活动特征及其与红河断裂的关系[J]. 地质力学学报, 22(3): 517-530. doi: 10.3969/j.issn.1006-6616.2016.03.009

    CrossRef Google Scholar

    陈文寄, 李齐, 汪一鹏, 1996. 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, 42(5): 385-390. doi: 10.3321/j.issn:0371-5736.1996.05.001

    CrossRef Google Scholar

    国家地震局地质研究所和云南省地震局. 1990. 滇西北地区活动断裂[M]. 北京: 地震出版社: 1-321.

    Google Scholar

    虢顺民, 向宏发, 计凤桔, 等, 1996. 红河断裂带第四纪右旋走滑与尾端拉张转换关系研究[J]. 地震地质, 18(4): 301-309.

    Google Scholar

    虢顺民, 计凤桔, 向宏发, 等, 2001. 红河活动断裂带[M]. 北京: 海洋出版社: 1-172.

    Google Scholar

    韩竹军, 向宏发, 虢顺民, 2005. 滇西北丽江盆地北部区第四纪时期的左旋剪切拉张[J]. 科学通报, 50(4): 356-362. doi: 10.3321/j.issn:0023-074X.2005.04.010

    CrossRef Google Scholar

    黄小巾, 吴中海, 李家存, 等, 2014. 滇西北裂陷带的构造地貌特征与第四纪构造活动性[J]. 地质通报, 33(4): 578-593. doi: 10.3969/j.issn.1671-2552.2014.04.013

    CrossRef Google Scholar

    黄小巾, 吴中海, 黄小龙, 等, 2018. 滇西北程海-宾川断裂带第四纪分段活动性的构造地貌表现与限定[J]. 地球科学, 43(12): 4651-4670.

    Google Scholar

    黄小龙, 吴中海, 吴坤罡, 等, 2016. 滇西北永胜地区主要活动断裂与活动构造体系[J]. 地质力学学报, 22(3): 531-547. doi: 10.3969/j.issn.1006-6616.2016.03.010

    CrossRef Google Scholar

    黄小龙, 吴中海, 刘锋, 等, 2021. 滇西北程海断裂带主要古地震滑坡及其分布特征的构造解释[J]. 地学前缘, 28(2): 125-139.

    Google Scholar

    李光容, 金德山, 1990. 程海断裂带挽近期活动性研究[J]. 云南地质, 9(1): 1-24.

    Google Scholar

    李玶, 汪良谋, 1975. 云南川西地区地震地质基本特征的探讨[J]. 地质科学, 10(4): 308-326.

    Google Scholar

    刘光勋, 李方全, 李桂荣, 1986. 我国滇西北地震活动区的活动构造与应力状态[J]. 地震地质, 8(1): 1-14.

    Google Scholar

    罗睿洁, 吴中海, 黄小龙, 等, 2015. 滇西北宾川地区主要活动断裂及其活动构造体系[J]. 地质通报, 34(1): 155-170. doi: 10.3969/j.issn.1671-2552.2015.01.013

    CrossRef Google Scholar

    潘桂棠, 肖庆辉, 陆松年, 等, 2009. 中国大地构造单元划分[J]. 中国地质, 36(1): 1-28.

    Google Scholar

    钱晓东, 苏有锦, 付虹, 等, 2011. 2011年云南盈江5.8级地震及震前短临跟踪预测[J]. 地震研究, 34(4): 403-413. doi: 10.3969/j.issn.1000-0666.2011.04.001

    CrossRef Google Scholar

    吴大宁, 邓起东, 1985. 滇西北裂陷区的基本特征及其形成机制[M]//国家地震局地质研究所. 现代地壳运动研究-1-大陆裂谷与深部过程. 北京: 地震出版社: 118-132.

    Google Scholar

    吴中海, 龙长兴, 范桃园, 等, 2015. 青藏高原东南缘弧形旋扭活动构造体系及其动力学特征与机制[J]. 地质通报, 34(1): 1-31. doi: 10.3969/j.issn.1671-2552.2015.01.002

    CrossRef Google Scholar

    向宏发, 虢顺民, 冉勇康, 等, 1986. 滇西北地区的现代构造应力场[J]. 地震地质, 8(1): 15-23.

    Google Scholar

    向宏发, 虢顺民, 徐锡伟, 等, 2000. 川滇南部地区活动地块划分与现今运动特征初析[J]. 地震地质, 22(3): 253-264. doi: 10.3969/j.issn.0253-4967.2000.03.006

    CrossRef Google Scholar

    向宏发, 韩竹军, 虢顺民, 陈立春, 张晚霞. 2004. 红河断裂带大型右旋走滑运动定量研究的若干问题[J]. 地球科学进展, (S1): 56-59.

    Google Scholar

    肖坤泽, 童亨茂, 2020. 走滑断层研究进展及启示[J]. 地质力学学报, 26(2): 151-166.

    Google Scholar

    徐锡伟, 闻学泽, 郑荣章, 等, 2003. 川滇地区活动块体最新构造变动样式及其动力来源[J]. 中国科学D辑: 地球科学, 33(S1): 151-162.

    Google Scholar

    云南省地质矿产局, 1990. 云南省区域地质志[M]. 北京: 中国地质出版社: 1-728.

    Google Scholar

    张建国, 皇甫岗, 谢英情, 等, 2009. 越南红河断裂活动性研究[J]. 地震地质, 31(3): 389-400. doi: 10.3969/j.issn.0253-4967.2009.03.002

    CrossRef Google Scholar

    郑文俊, 张培震, 袁道阳, 等, 2019. 中国大陆活动构造基本特征及其对区域动力过程的控制[J]. 地质力学学报, 25(5): 699-721.

    Google Scholar

    中国人民解放军建字七三〇部队. 1978. 1: 20万大理幅水文地质普查成果报告[Z].

    Google Scholar

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