青藏高原东南缘上地壳晚新生代构造变形综述

计昊旻; 任治坤; 刘金瑞

doi:10.3799/dqkx.2023.160

Volume 49 Issue 2

Feb. 2024

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2024 > 49(2): 480-499

Ji Haomin, Ren Zhikun, Liu Jinrui, 2024. Review of Structural Deformation in the Upper Crust of the Southeastern Margin of the Tibetan Plateau since the Late Cenozoic. Earth Science, 49(2): 480-499. doi: 10.3799/dqkx.2023.160

Citation:

Ji Haomin, Ren Zhikun, Liu Jinrui, 2024. Review of Structural Deformation in the Upper Crust of the Southeastern Margin of the Tibetan Plateau since the Late Cenozoic. Earth Science, 49(2): 480-499. doi: 10.3799/dqkx.2023.160

Citation:

PDF( 13021 KB)

Review of Structural Deformation in the Upper Crust of the Southeastern Margin of the Tibetan Plateau since the Late Cenozoic

doi: 10.3799/dqkx.2023.160

Ji Haomin^{1, 2
,
,},
Ren Zhikun^{1, 2
,
,
,},
Liu Jinrui^{1, 2}

1.
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
2.
Key Laboratory of Seismic and Volcanic Hazards, China Earthquake Administration, Beijing 100029, China

Received Date: 2023-01-15
Publish Date: 2024-02-25

Abstract

Abstract

The southeastern margin of the Tibetan Plateau is an ideal experimental field to test the evolutionary model of the Tibetan Plateau and one of the most seismically active regions in the world. In this paper, we review the decadal and 10, 000⁃year⁃scale slip habits of the major active faults on the southeastern margin of the Tibetan Plateau and the 100⁃year⁃scale regional seismic activity, combined with the million⁃year time⁃scale chronology studies, we think the internal material of the Tibetan Plateau gradually flowed out to the east and was blocked by the Sichuan Basin, turning to the southeastern margin area for clockwise rotational movement since the middle and late Miocene. In the Late Quaternary, the upper crustal deformation in the southeastern margin has changed from being concentrated in large strike⁃slip boundary faults and thrust fold belts to being diffusely distributed to secondary faults in the region, forming the kinematic characteristics of clockwise rotation around the eastern Himalayan syntaxis with the Xianshuihe⁃Xiaojiang Fault Zone and the Sagaing Fault Zone as boundaries. Accordingly, the deformation of the southeastern margin of the Tibetan Plateau can be divided into two stages. The deformation of the early Miocene period was concentrated in large boundary faults, which conforms to the deformation of rigid blocks, and turned into diffuse continuous deformation in the late Quaternary. Based on the comparison of horizontal slip rate, seismogenic capacity and seismic activity, the active faults on the southeast edge of the Tibetan Plateau can be roughly divided into three levels. The first⁃tier faults are the boundary fault Xianshuihe⁃Xiaojiang fault zone and Sagaing fault zone, with horizontal slip rates ≥10 mm/a, capable of occurring earthquakes of M 8 and above alone, and can continuously generate strong earthquakes of M 7⁃7.9, which are the first⁃tier tectonic frame since the Late Quaternary in the southeastern margin; the second⁃tier faults can control the strongly active tectonic units in the southeast margin, with horizontal slip rates ~3⁃6 mm/a, generally capable of occurring earthquakes of M 7⁃7.9, and can continuously generate earthquakes of M 6⁃6.9; the horizontal slip rate of Level 3 faults is generally ≤2 mm/a, they are only capable to generating earthquakes less to M 7, and are generally smaller in scale but more numerous. In addition, the Late Quaternary deformation characteristics of the Chuandian Block have changed from the original slip movement along the large boundary faults to the rotation, translation and differential uplift of the secondary active blocks around the Xianshuihe⁃Xiaojiang Fault Zone.
- the southeastern margin of the Tibetan Plateau,
- upper crust deformation characteristics,
- diffusion deformation,
- faults classification,
- earthquake

FullText(HTML)

References(96)

References

Akciz, O. S., 2004. Structure and Geochronological Constraints on the Ductile Deformation Observed along the Gaoligong Shan and Chong Shan Shear Zones, Yunnan (China)(Dissertation). Massachusetts Institute of Technology, Cambridge.

Allen, C. R., Gillespie, A. R., Han, Y., et al., 1984. Red River and Associated Faults, Yunnan Province, China: Quaternary Geology, Slip Rates, and Seismic Hazard. Geological Society of America Bulletin, 95(6): 686. https://doi.org/10.1130/0016⁃7606(1984)95686: rraafy>2.0.co;2 doi: 10.1130/0016⁃7606(1984)95686:rraafy>2.0.co;2

An, Z., Zhang, P., Wang, E., et al., 2006. Changes of the Monsoon⁃Arid Environment in China and Growth of the Tibetan Plateau Since the Miocene. Quaternary Sciences, 26(5): 1-16 (in Chinese with English abstract).

Avouac, J. P., Tapponnier, P., 1993. Kinematic Model of Active Deformation in Central Asia. Geophysical Research Letters, 20(10): 895-898. https://doi.org/10.1029/93gl00128

Bai, M. K., Chevalier, M. L., Leloup, P. H., et al., 2021. Spatial Slip Rate Distribution along the SE Xianshuihe Fault, Eastern Tibet, and Earthquake Hazard Assessment. Tectonics, 40(11): e2021TC006985. https://doi.org/10.1029/2021tc006985

Bai, M., Chevalier, M. L., Pan, J., et al., 2018. Southeastward Increase of the Late Quaternary Slip⁃Rate of the Xianshuihe Fault, Eastern Tibet, Geodynamic and Seismic Hazard Implications. Earth and Planetary Science Letters, 485: 19-31. https://doi.org/10.1016/j.epsl.2017.12.045.

Chang, Y., Chen, L., Zhang, Q., 2019. Study on the Tectonic Landform and Fault Activity Characteristics of the Jinsha River Fault Zone. International Earthquake Dynamics, 8 (13): 142-143 (in Chinese).

Chen, G. F., Bartholomew, M., Liu, D. M., et al., 2022. Paleo-Earthquakes along the Zheduotang Fault, Xianshuihe Fault System, Eastern Tibet: Implications for Seismic Hazard Evaluation. Journal of Earth Science, 33(5): 1233-1245. https://doi.org/10.1007/s12583⁃022⁃1687⁃0

Chen, G., Xu, X., Wen, X., et al. 2016. Late Quaternary Slip⁃Rates and Slip⁃Partitioning on the Southeastern Xianshuihe Fault System, Eastern Tibetan Plateau. Acta Geologica Sinica (English Edition), 90: 537-554. https://doi.org/10.1111/1755⁃6724.12689

Deng, J., Wang, Q. F., Li, G. J., et al., 2014. Cenozoic Tectono⁃Magmatic and Metallogenic Processes in the Sanjiang Region, Southwestern China. Earth⁃Science Reviews, 138: 268-299. https://doi.org/10.1016/j.earscirev.2014.05.015

Deng, Q., Zhang, P., Ran, Y., et al., 2002. Basic Characteristics of Activity Structure in Mainland China. Chinese Science: Earth Science, 32: 1020-1030(in Chinese with English abstract).

Department of Earthquake Disaster Prevention, China Earthquake Administration, 1995. Catalogue of Strong Earthquakes in Chinese History: 23rd Century BC~1911 AD. Seismological Press, Beijing(in Chinese).

Department of Earthquake Disaster Prevention, China Earthquake Administration, 1999. Catalogue of Modern Earthquakes in China: AD 1912—1990, Ms≥4.7. China Science and Technology Press, Beijing (in Chinese).

England, P., Houseman, G., 1986. Finite Strain Calculations of Continental Deformation: 2. Comparison with the India⁃Asia Collision Zone. Journal of Geophysical Research: Solid Earth, 91(B3): 3664-3676. https://doi.org/10.1029/jb091ib03p03664

England, P., Houseman, G., 1988. The Mechanics of the Tibetan Plateau. Philosophical Transactions of the Royal Society of London Series A, Mathematical and Physical Sciences, 326(1589): 301-320. https://doi.org/10.1098/rsta.1988.0089

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. International Geology Review, 48(4): 287-310. https://doi.org/10.2747/0020⁃6814.48.4.287

Flesch, L. M., Haines, A. J., Holt, W. E., 2001. Dynamics of the India⁃Eurasia Collision Zone. Journal of Geophysical Research: Solid Earth, 106(B8): 16435-16460. https://doi.org/10.1029/2001jb000208

Gan, W. J., Zhang, P. Z., Shen, Z. K., et al., 2007. Present⁃Day Crustal Motion within the Tibetan Plateau Inferred from GPS Measurements. Journal of Geophysical Research: Solid Earth, 112(B8): B08416. https://doi.org/10.1029/2005jb004120

Gan, W., Molnar, P., Zhang, P., et al., 2021. Initiation of Clockwise Rotation and Eastward Transport of Southeastern Tibet Inferred from Deflected Fault Traces and GPS Observations. Geological Society of America Bulletin, (5/6): 134. https://doi.org/10.1130/B36069.1

Gao, Y., Ding, R., Zhang, S., et al., 2019. Slip Rate of Lijiang⁃Xiaojinhe Fault in the Holocene. Technology for Earthquake Disaster Prevention, (3): 617-627(in Chinese with English abstract).

He, H., Oguchi, T., 2008. Late Quaternary Activity of the Zemuhe and Xiaojiang Faults in Southwest China from Geomorphological Mapping. Geomorphology, 96(1/2): 62-85. https://doi.org/10.1016/j.geomorph.2007.07.009

He, H., Yasutakyr, I., 2007. Faulting on the Anninghe Fault Zone, Southwest China in Late Quaternary and Its Movement Model. Acta Seismologica Sinica, 29(5): 537-548 (in Chinese with English abstract).

He, Y., Zhou, R., Li, X., et al., 2001. Seismic Rupture and Source Stress Field of Gengma M7.2 Earthquake in Yunnan Province. North China Earthquake Sciences, 19(2): 21-26 (in Chinese with English abstract).

Hu, M., Wu, Z., Li, J., et al. 2021. Late Quaternary Left⁃Lateral Strike Slip Rate along the Anninghe⁃Zemuhe Section of the Xianshuihe⁃Xiaojiang Fault System and Its Implication to the Clockwise Block Rotation of the SE Margin of the Tibetan Plateau. Geochemistry, Geophysics, Geosystems, https://doi.org/10.1002/essoar.10505860.2.

Institute of Geology, State Seismological Administration and Seismological Administration of Yunnan Province, 1990. Active Faults in Northwest Yunnan. Seismological Press, Beijing (in Chinese).

Jiao, L. Q., Tapponnier, P., Donzé, F. V., et al., 2023. Discrete Element Modeling of Southeast Asia's 3D Lithospheric Deformation during the Indian Collision. Journal of Geophysical Research: Solid Earth, 128(1): e2022JB025578. https://doi.org/10.1029/2022jb025578

Lacassin, R., Replumaz, A., Hervé Leloup, P., 1998. Hairpin River Loops and Slip⁃Sense Inversion on Southeast Asian Strike⁃Slip Faults. Geology, 26(8): 703. https://doi.org/10.1130/0091⁃7613(1998)0260703: hrlass>2.3.co;2 doi: 10.1130/0091⁃7613(1998)0260703:hrlass>2.3.co;2

Leloup, P. H., Arnaud, N., Lacassin, R., et al., 2001. New Constraints on the Structure, Thermochronology, and Timing of the Ailao Shan⁃Red River Shear Zone, SE Asia. Journal of Geophysical Research: Solid Earth, 106(B4): 6683-6732. https://doi.org/10.1029/2000jb900322

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. Journal of Geophysical Research: Solid Earth, 98(B4): 6715-6743. https://doi.org/10.1029/92jb02791

Leloup, P. H., Lacassin, R., Tapponnier, P., et al., 1995. The Ailao Shan⁃Red River Shear Zone (Yunnan, China), Tertiary Transform Boundary of Indochina. Tectonophysics, 251(1/2/3/4): 3-84. https://doi.org/10.1016/0040⁃1951(95)00070⁃4

Leloup, P. H., Tapponnier, P., Lacassin, R., et al., 2007. Discussion on the Role of the Red River Shear Zone, Yunnan and Vietnam, in the Continental Extrusion of SE Asia. Journal of the Geological Society, 164(6): 1253-1260. https://doi.org/10.1144/0016⁃76492007⁃065

Li, C., Wang, Y., Gan, W., et al., 2020. Diffuse deformation in the SE Tibetan Plateau: New Insights from Geodetic Observations. Journal of Geophysical Research: Solid Earth, 125: e2020JB019383. https://doi.org/10.1029/2020JB019383

Liu⁃Zeng, J., Tapponnier, P., Gaudemer, Y., et al., 2008. Quantifying Landscape Differences across the Tibetan Plateau: Implications for Topographic Relief Evolution. Journal of Geophysical Research: Earth Surface, 113(F4): F04018. https://doi.org/10.1029/2007jf000897

Mitchell, A. H. G., 1993. Cretaceous⁃Cenozoic Tectonic Events in the Western Myanmar (Burma)⁃Assam Region. Journal of the Geological Society, 150(6): 1089-1102. https://doi.org/10.1144/gsjgs.150.6.1089

Peltzer, G., Tapponnier, P., 1988. Formation and Evolution of Strike⁃Slip Faults, Rifts, and Basins during India⁃Asia Collision: an Experiment Approach. Journal of Geophysical Research, 93: 15085-15117. https://doi.org/10.1029/JB093iB12p15085

Ran, Y., Cheng, J., Gong, H., et al., 2008. Late Quaternary Geomorphic Deformation and Displacement Rates of the Anninghe Fault around Zimakua. Seismology and Geology, 30 (1): 86-98(in Chinese with English abstract).

Ren, J., 1994. Late Quaternary Displacement and Slip Rate of Zemuhe Fault in Sichuan, China. Seismology and Geology, 16(2): 146(in Chinese with English abstract).

Replumaz, A., Lacassin, R., Tapponnier, P., et al., 2001. Large River Offsets and Plio⁃Quaternary Dextral Slip Rate on the Red River Fault (Yunnan, China). Journal of Geophysical Research: Solid Earth, 106(B1): 819-836. https://doi.org/10.1029/2000jb900135

Schoenbohm, L. M., Burchfiel, B. C., Chen, L. Z., 2006b. Propagation of Surface Uplift, Lower Crustal Flow, and Cenozoic Tectonics of the Southeast Margin of the Tibetan Plateau. Geology, 34(10): 813. https://doi.org/10.1130/g22679.1

Schoenbohm, L. M., Burchfiel, B. C., Liangzhong, C., et al., 2006a. Miocene to Present Activity along the Red River Fault, China, in the Context of Continental Extrusion, Upper⁃Crustal Rotation, and Lower⁃Crustal Flow. Geological Society of America Bulletin, 118(5/6): 672-688. https://doi.org/10.1130/b25816.1

Searle, M. P., Noble, S. R., Cottle, J. M., et al., 2007. Tectonic Evolution of the Mogok Metamorphic Belt, Burma (Myanmar) Constrained by U⁃Th⁃Pb Dating of Metamorphic and Magmatic Rocks. Tectonics, 26(3): TC3014. https://doi.org/10.1029/2006tc002083

Shen, Z. K., Lü, J. N., Wang, M., et al., 2005. Contemporary Crustal Deformation around the Southeast Borderland of the Tibetan Plateau. Journal of Geophysical Research: Solid Earth, 110(B11): 409. https://doi.org/10.1029/2004jb003421

Shi, X. H., Wang, Y., Sieh, K., et al., 2018a. Fault Slip and GPS Velocities across the Shan Plateau Define a Curved Southwestward Crustal Motion around the Eastern Himalayan Syntaxis. Journal of Geophysical Research: Solid Earth, 123(3): 2502-2518. https://doi.org/10.1002/2017jb015206

Shi, X. H., Sieh, K., Weldon, R., et al., 2018b. Slip Rate and Rare Large Prehistoric Earthquakes of the Red River Fault, Southwestern China. Geochemistry, Geophysics, Geosystems, 19(7): 2014-2031. https://doi.org/10.1029/2017gc007420

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. Nature, 343(6257): 431-437. https://doi.org/10.1038/343431a0

Tin, T., Nishimura, T., Hashimoto, M., et al. 2022. Present⁃Day Crustal Deformation and Slip Rate along the Southern Sagaing Fault in Myanmar by GNSS Observation. Journal of Asian Earth Sciences, 228: 105125. https://doi.org/10.1016/j.jseaes.2022.105125

Wang, D., Dong, Y., Jiao, Q., et al., 2022. The Mechanism of Tectonic Deformation of the Central Yunnan Terrane in the Late Cenozoic Based on Tectonic Geomorphology. Earth Science, 47(8): 3016-3028(in Chinese with English abstract).

Wang, E., Kirby, E., Furlong, K. P., et al., 2013. Two⁃Phase Growth of High Topography in Eastern Tibet during the Cenozoic. Nature Geoscience, 5(9): 640-645. https://doi.org/10.1038/ngeo1538

Wang, H., Ran, Y., Chen, L., et al., 2018. Determination of Slip Rate on the Southern Segment of the Anninghe Fault. Seismology and Geology, 40 (5): 967-979 (in Chinese with English abstract).

Wang, H., Yang, Z. Y., Jing, L. Z., et al., 2023. Tectonic Rotation Pattern at the Northern End of the Red River Fault System in SE Tibet: New Paleomagnetic Evidence from Cretaceous Red Beds. Tectonics, 42(3): e2021TC007116. https://doi.org/10.1029/2021tc007116

Wang, M., Shen, Z. K., 2020. Present⁃Day Crustal Deformation of Continental China Derived from GPS and Its Tectonic Implications. Journal of Geophysical Research: Solid Earth, 125(2): e2019JB018774. https://doi.org/10.1029/2019jb018774

Wang, Y., Sieh, K., Tun, S., et al., 2014. Active Tectonics and Earthquake Potential of the Myanmar Region. Journal of Geophysical Research: Solid Earth, 119: 3767-3822. https://doi.org/10.1002/2013JB010762

Wang, Y., Wang, E., Shen, Z., et al., 2008. Inversion of Current Activity Rates of Major Faults in Sichuan⁃Yunnan Region Based on GPS Data Constraints. Science China Earth Sciences, 38(5): 582-597 (in Chinese with English abstract).

Wang, Y., Wang, Y. J., Zhang, P. Z., et al., 2019. Intracontinental Deformation within the India⁃Eurasia Oblique Convergence Zone: Case Studies on the Nantinghe and Dayingjiang Faults. GSA Bulletin, 132(3/4): 850-862. https://doi.org/10.1130/b35338.1

Wang, Y., Zhang, B., Hou, J., et al., 2015. Late Quaternary Activity of the Qujiang Fault and Analysis of the Slip Rate. Seismology and Geology, 37 (4): 1177-1192(in Chinese with English abstract).

Wei, Z., He, H., Shi, F., et al., 2012. Slip Rate on the South Segment of Daliangshan Fault zone. Seismology and Geology, 34(2): 282-293 (in Chinese with English abstract).

Xu, X., Wen, X., Zheng, R., et al., 2003. Newly Tectonic Deformation and its Dynamic Source of the Sichuan⁃Yunnan Block. Science in China (Ser D), 33(4): 151-162(in Chinese with English abstract).

Xu, Z., Yang, J., Li, H., et al., 2011. On the Tectonics of the India⁃Asia Collision. Acta Geologica Sinica, (1): 1-33(in Chinese with English abstract).

Yin, A., Harrison, T. M., 2000. Geologic Evolution of the Himalayan⁃Tibetan Orogen. Annual Review of Earth and Planetary Sciences, 28: 211-280. https://doi.org/10.1146/annurev.earth.28.1.211

Zhang, B., Zhang, J., Zhong, D., 2010. Structure, Kinematics and Ages of Transpression during Strain⁃Partitioning in the Chongshan Shear Zone, Western Yunnan, China. Journal of Structural Geology, 32(4): 445-463. https://doi.org/10.1016/j.jsg.2010.02.001

Zhang, B., Zhang, J., Zhong, D., et al., 2012. Poly Stage Deformation of the Gaoligong Metamorphic Zone: Structures, ⁴⁰Ar/³⁹Ar Mica Ages, and Tectonic Implications. Journal of Structural Geology, 37: 1-18. https://doi.org/10.1016/j.jsg.2012.02.007

Zhang, G., Tian, Y., Li, R., et al, . 2022. Progressive Tectonic Evolution from Crustal Shortening to Mid⁃Lower Crustal Expansion in the Southeast Tibetan Plateau: A Synthesis of Structural and Thermochronological Insights. Earth⁃Science Reviews, 226: 103951. https://doi.org/10.1016/j.earscirev.2022.103951

Zhang, G., Zhang, P., 2000. Medium⁃Term Academic Progress of "Mechanism and Prediction of Strong Earthquakes in Mainland". Basic Science in China, 10: 4-10 (in Chinese).

Zhang, P., Deng, Q., Zhang, G., et al., 2003. Strong Earthquake Activity and Active Blocks in Mainland China. China Science Series D: Earth Science, 33 (Supplement): 12-20 (in Chinese).

Zhang, P., Deng, Q., Zhang, Z., et al., 2013. Active Faults, Earthquake Hazards and Associated Geodynamic Processes in Continental China. Scientia Sinica Terrae, 43(10): 1607-1620 (in Chinese with English abstract). doi: 10.1360/zd-2013-43-10-1607

Zhang, P., Shen, Z, Wang, M, et al., 2004. Continuous Deformation of the Tibetan Plateau from Global Positioning System Data. Geology, 32(9): 809-812. https://doi.org/10.1130/G20554.1

Zhang, P., Wang, W., Gan, W., et al. 2022. Present⁃Day Deformation and Geodynamic Processes of the Tibetan Plateau. Acta Geologica Sinica, 96(10): 3297-3313. (in Chinese with English abstract).

Zhang, Y., Yao, X., Yu, K., et al. 2016. Late Quaternary Slip-Rate and Seismic Activity of the Xianshuihe Fault Zone in Southwest China. Acta Geologica Sinica (English Edition). 90: 525-536. https://doi.org/10.1111/1755⁃6724.12688

Zhou, R., Ma, S., Cai, C., 1996. Late Quaternary Active Features of the Ganzi⁃Yushu Fault Zone. Earthquake Research in China, 12(3): 250-260(in Chinese with English abstract).

Zhu, L., 2020. Numerical Simulation of Crustal Deformation Dynamics in the Southeastern Margin of the Tibetan Plateau(Dissertation). Institute of Geology, China Earthquake Administration, Beijing (in Chinese with English abstract).

安芷生, 张培震, 王二七, 等, 2006. 中新世以来我国季风-干旱环境演化与青藏高原的生长. 第四纪研究, 26(5): 1-16. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200605001.htm

常玉巧, 陈立春, 张琦, 2019. 金沙江断裂带构造地貌与断裂活动特征研究. 国际地震动态, 8(13): 142-143. https://www.cnki.com.cn/Article/CJFDTOTAL-GJZT201908115.htm

邓起东, 张培震, 冉勇康, 等, 2002. 中国大陆活动构造基本特征. 中国科学D辑: 地球科学, 32: 1020-1030. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201905007.htm

郜宇, 丁锐, 张世民, 等, 2019. 丽江-小金河断裂全新世滑动速率研究. 震灾防御技术, (3): 617-627. https://www.cnki.com.cn/Article/CJFDTOTAL-ZZFY201903014.htm

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. 北京: 地震出版社.

何宏林, 池田安隆, 2007. 安宁河断裂带晚第四纪运动特征及模式的讨论. 地震学报, 29(5): 537-548. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXB200705012.htm

何玉林, 周荣军, 黎小刚, 等, 2001. 云南耿马7.2级地震破裂与震源应力场. 华北地震科学, 19(2): 21-26. https://www.cnki.com.cn/Article/CJFDTOTAL-HDKD200102003.htm

冉勇康, 程建武, 宫会玲, 等, 2008. 安宁河断裂紫马跨一带晚第四纪地貌变形与断层位移速率. 地震地质, 30(1): 86-98. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200801006.htm

任金卫, 1994. 则木河断裂晚第四纪位移及滑动速率. 地震地质, 16(2): 146. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ402.006.htm

邵志刚, 冯蔚, 王芃, 等, 2020. 中国大陆活动地块边界带的地震活动特征研究综述. 地震地质, 42(2): 271-282. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ202002003.htm

王丹, 董有浦, 焦骞骞, 等, 2022. 滇中地块新生代晚期的变形机制: 基于构造地貌学分析. 地球科学, 47(8): 3016-3028. doi: 10.3799/dqkx.2021.146

王虎, 冉永康, 陈立春, 等, 2018. 安宁河断裂带南段滑动速率估计. 地震地质, 40(5): 967-979. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201805003.htm

王阎昭, 王恩宁, 沈正康, 等, 2008. 基于GPS资料约束反演川滇地区主要断裂现今活动速率. 中国科学D辑: 地球科学, 38(5): 582-597. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200805006.htm

王洋, 王岳军, 张培震, 等, 2022. 青藏高原东南缘断裂体系新生代构造演化. 中国科学: 地球科学, 52(5): 777-802. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK202205001.htm

王洋, 张波, 侯建军, 等, 2015. 曲江断裂晚第四纪活动特征及滑动速率分析. 地震地质, 37(4): 1177-1192. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201504019.htm

魏占玉, 何宏林, 石峰等, 2012. 大凉山断裂带南段滑动速率估计. 地震地质, 34(2): 282-293. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201202008.htm

徐锡伟, 闻学泽, 郑荣章等. 2003. 川滇地区活动地块最新构造变动样式及其动力来源. 中国科学: D辑, 33(4): 151-162. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2003S1016.htm

许志琴, 杨经绥, 李海兵, 等, 2011. 印度-亚洲碰撞大地构造. 地质学报(1): 1-33. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201101001.htm

张国民, 张培震, 2000. "大陆强震机理与预测"中期学术进展. 中国基础科学, 10: 4-10 https://www.cnki.com.cn/Article/CJFDTOTAL-ZGJB200010000.htm

张培震, 邓起东, 张国民, 等, 2003. 中国大陆强震活动与活动地块. 中国科学D辑: 地球科学, 33(增刊): 12-20. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200407000.htm

张培震, 邓起东, 张竹琪, 等, 2013. 中国大陆的活动断裂、地震灾害及其动力过程. 中国科学: 地球科学, 43(10): 1607-1620. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201310005.htm

张培震, 王伟涛, 甘卫军, 等, 2022. 青藏高原的现今构造变形与地球动力过程. 地质学报, 96(10): 3297-3313. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE202210002.htm

中国地震局震害防御司, 1995. 中国历史强震目录: 公元前23世纪—公元1911年. 北京: 地震出版社.

中国地震局震害防御司, 1999. 中国近代地震目录: 公元1912年—1990年, Ms≥4.7. 北京: 中国科学技术出版社.

周荣军, 黎小刚, 黄祖智, 等, 2003. 四川大凉山断裂带的晚第四纪平均滑动速率. 地震研究, 26 (2): 191-196. https://www.cnki.com.cn/Article/CJFDTOTAL-DZYJ200302013.htm

朱良玉, 2020. 青藏高原东南缘地壳形变动力学数值模拟研究(博士学位论文). 北京: 中国地震局地质研究所.

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(6) / Tables(3)

Get Citation

PDF

XML

Article views (653) PDF downloads(163)

Review of Structural Deformation in the Upper Crust of the Southeastern Margin of the Tibetan Plateau since the Late Cenozoic

doi: 10.3799/dqkx.2023.160

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content