2017年四川九寨沟<i>M</i><sub>s</sub>7.0地震InSAR同震形变场及发震构造探讨

姚鑫; 周振凯; 李凌婧; 刘星洪; 姚佳明

2017年四川九寨沟M_s7.0地震InSAR同震形变场及发震构造探讨

姚鑫^{1, 2,},
周振凯^{1, 2},
李凌婧^{1, 2},
刘星洪^{1, 2, 3},
姚佳明⁴

1.
国土资源部新构造运动与地质灾害重点实验室, 北京 100081
2.
中国地质科学院地质力学研究所, 北京 100081
3.
中国地质大学(北京)地球科学与资源学院, 北京 100083
4.
中国地质大学(北京)工程技术学院, 北京 100083

基金项目:

国家自然科学基金项目 41672359

中国地质调查局工作项目 DD20179282

中国地质调查局工作项目 DD20160272

中央级公益性科研院所基本科研业务费项目 DZLXJK201611

详细信息

作者简介:
姚鑫(1978-), 男, 教授级高工, 主要从事地质灾害与InSAR研究.E-mail:yaoxinphd@163.com

中图分类号: P315.2
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- 被引次数: 0
出版历程
- 收稿日期: 2017-08-22
- 刊出日期: 2017-08-01

INSAR CO-SEISMIC DEFORMATION OF 2017 M_s 7.0 JIUZHAIGOU EARTHQUAKE AND DISCUSSIONS ON SEISMOGENIC TECTONICS

YAO Xin^{1, 2
,},
ZHANG Zhenkai^{1, 2},
LI Lingjing^{1, 2},
LIU Xinghong^{1, 2, 3},
YAO Jiaming⁴

1.
Key Laboratory of Neotectonic Movement & Geohazards, Ministry of Land and Mineral Resources, Beijing 100081, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
4.
School of Engineering and Technology, Chinese University of Geosciences (Beijing), Beijing 100083, China

摘要

摘要: 2017年8月8日四川省九寨沟县发生M_s7.0级地震，构造部位处于青藏高原东缘的巴颜喀拉地块东北角，震中位置是岷江断裂、塔藏断裂、虎牙断裂和雪山梁子断裂围闭的空震区。哪条断裂发震，如何界定其与周边活动断裂的关系，与青藏高原东缘近年来发生的大地震是否有成因联系等问题对于理解该区域现今构造活动模式、预判地震发展趋势和部署地震地质灾害防控等工作具有重要意义。利用地震前后两期Sentinel-1合成孔径雷达数据对地表同震形变场进行了InSAR测量，获取了极震区约2000 km²范围内的雷达视线向变形（-13~28 cm）和运动方向，呈现为主动盘单侧走滑兼逆冲的变形模式，结合震源机制、断裂展布、构造背景和近年地震迁移的分析，揭示了控震构造是巴颜喀拉地块北缘边界断裂弧形旋转体系的尾端构造，发震断层是该断裂系中塔藏断裂的南段，并有与虎牙断裂贯通的趋势，因此，应重视本次地震与虎牙断裂之间的空震区未来的强震危险性问题；从区域上看，此次九寨沟地震可能与汶川地震具有一定的时空成因联系，因在巴颜喀拉地块南北边界断裂破裂基本贯通的条件下，2008年汶川地震诱发的东缘中部锁固破裂导致块体加速向东挤出，2013年鲁甸地震又释放了东缘南段挤压构造应力，从而进一步加剧了东北角的应力集中，促使九寨沟地震的发生。
- 九寨沟地震 /
- 干涉雷达 /
- 巴颜喀拉地块 /
- 塔藏断裂
Abstract: An M_s7.0 earthquake occurred in Jiuzhaigou county on Aug. 8, 2017. Tectonic location is the NE part of Bayan-Har block, with epicenter in the earthquake-free zone surrounded by Minjiang fault, Tazang fault, Huya fault as well as Xueshanliangzi fault, and where is of free earthquake zone. Which is the seismogenic fault? How to define the relationship between this earthquake and the neighbor faults? Does it have the causal association with huge earthquakes in recent years? The answers to those questions are of great significance to understand the current tectonic activity pattern, predict seismic development trend and deploy earthquake geological disaster prevention and control. Using two periods of Sentinel-1 SAR data to carry out InSAR survey, co-seismic deformation (-13~28 cm) and movement direction within 2000 km² in meizoseismal area were measured, showing passive singe wall strike-slip and thrust ground deformation. Based on analysis of focal mechanism solution, fault distribution, tectonic background and recent seismic migration, conclusions are made as follows. The seismogenic structure is the end structure of an arc rotation system in northeastern boundary of Bayan-Har block, and the seismogenic fault is the southern branch of Tazang fault, with the trend to connect with Huya fault, therefore, the section between them should be paid more attention to in the future. There are certain spatio-temporal genetic relation between Jiuzhaigou earthquake and Wenchuan earthquake: in condition of ruptures existed in north and south boundary of Bayan-Har block, the 2008 Wenchuan earthquake induced new rupture in east edge to accelerate block eastward extrusion, and 2013 Ludian earthquake released tectonic stress in southern section, further exacerbating stress concentration in northeastern angle, which led to the 2017 Jiuzhaigou earthquake.
- Jiuzhaigou earthquake /
- InSAR /
- Bayan-Har block /
- Tazang fault

HTML全文

图 1 干涉雷达测量原理示意图

Figure 1. Schematic diagram of InSAR measurement

下载: 全尺寸图片幻灯片

图 2 九寨沟地震及活动构造背景

Figure 2. Jiuzhaigou earthquake and active tectonic setting

下载: 全尺寸图片幻灯片

图 3 两轨干涉+DEM差分干涉处理流程图

Figure 3. Flowchart of InSAR process with two orbits+DEM

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图 4 九寨沟地震同震形变InSAR缠绕条纹图

Figure 4. Wrapped InSAR strip image of Jiuzhaigou earthquake co-seismic deformation

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图 5 解缠后的九寨沟地震干涉雷达视线向绝对变形量

Figure 5. Unwrapped InSAR LOS Deformation of Jiuzhaigou earthquake

下载: 全尺寸图片幻灯片

图 6 单侧走滑兼逆冲型断裂活动地表变形模式

Figure 6. Singe wall strike-slipping and thrust fault as well as corresponding ground surface deformation

下载: 全尺寸图片幻灯片

图 7 巴颜喀拉地块活动诱发九寨沟地震机制示意图

Figure 7. Schematic diagram of Jiuzhaigou earthquake triggered by Bayan-Har block activity

下载: 全尺寸图片幻灯片

参考文献(15)

[1]	Zhang Y S, Yao X, Xiong T Y, et al. Rapid identification and emergency investigation of surface ruptures and geohazards induced by the M_s7.1 Yushu earthquake[J]. Acta Geologica Sinica, 2010, 84(6): 1315~1327. doi: 10.1111/acgs.2010.84.issue-6
[2]	姚鑫, 张永双, 杨农, 等.玉树地震地表变形InSAR观测及初步分析[J].地质力学学报, 2010, 16(2): 129~136. http://www.cnki.com.cn/article/cjfdtotal-dzlx201002004.htm YAO Xin, ZHANG Yongshuang, YANG Nong, et al. D-inSAR observation of earth surface deformation in the M_S7.1 Yushu earthquake[J]. Journal of Geomechanics, 2010, 16(2): 129~136. http://www.cnki.com.cn/article/cjfdtotal-dzlx201002004.htm
[3]	滕吉文, 刘财, 韩立国, 等.汶川—映秀M_S8.0地震的介质破裂与深部物质运移的动力机制[J].吉林大学学报(地球科学版), 2009, 39(4): 559~583. TENG Jiwen, LIU Cai, HAN Liguo, et al. The dynamical mechanism for medium rapture and motion of deep matler on Wenchuan—Yingxiu M_s8.0 earthquarce, 2008[J]. Journal of Jilin University (Earth Science Edition), 2009, 39(4): 559~583.
[4]	Yao X, Zhang Y S, Dai F C, et al. Geohazard distribution and geological activity of Wenchuan earthquake surveyed by D-InSAR[C]//Geological Active-International Association for Engineering Geology and Environment(IAEG) Congress 2010. [S.l.]Holand: CRC Press, 2010, 871~880.
[5]	Massonnet D, Rossi M, Carmona C, et al. The displacement field of the landers earthquake mapped by radar interferometry[J]. Nature, 1993, 364(6433): 138~142. doi: 10.1038/364138a0
[6]	张岳桥, 杨农, 施炜, 等.青藏高原东缘新构造及其对汶川地震的控制作用[J].地质学报, 2008, 82(12): 1668~1678. doi: 10.3321/j.issn:0001-5717.2008.12.004 ZHANG Yueqiao, YANG Nong, SHI Wei, et al. Neotectonics of eastern Tibet and its control on the Wenchuan earthquake[J]. Acta Geologica Sinica, 2008, 82(12): 1668~1678. doi: 10.3321/j.issn:0001-5717.2008.12.004
[7]	单斌, 熊熊, 金笔凯, 等.松潘—甘孜块体东北端强震间相互作用及地震危险性研究[J].地球物理学报, 2012, 55(7): 2329~2340, doi: 10.6038/j.issn.001~5733.2012. 07.018. SHAN Bin, XIONG Xiong, JIN Bikai, et al. Earthquake stress interaction in the northeastern Songpan-Garzê block and its implication for earthquake hazard[J]. Chinese Journal of Geophysics, 2012, 55(7): 2329~2340, doi: 10.6038/j.issn.001~5733.2012.07.018.
[8]	杜方, 苏有锦, 龙锋, 等.芦山7.0级、汶川8.0级地震与巴颜喀拉地块东缘区域历史地震[J].地球物理学进展, 2015, 30(4): 1569~1579, doi: 10.6038/pg20150411. DU fang, SU Youjin, LONG Feng, et al. TheM7.0 Lusha, the M8.0 Wenchuan earthquake and the history earthquakes in the eastern border area of the Bayan Har block[J]. Progress in Geophysics, 2015, 30(4): 1569~1579, doi: 10. 6038/pg20150411.
[9]	胡朝忠, 任金卫, 杨攀新, 等.东昆仑断裂东端塔藏断裂压剪活动与高原隆升作用讨论[J].地质学报, 2017, 91(7): 1401~1415. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201707002.htm HU Chaozhong, REN Jinwei, YANG Panxin, et al. Discussion on the Compression-shear activity of the Tazang fault in East Kunlun and Uplift of Plateau[J]. Acta Geologica Sinica, 2017, 91(7): 1401~1415. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201707002.htm
[10]	陈长云, 任金卫, 孟国杰, 等.巴颜喀拉块体北东缘主要断裂现今活动性分析[J].大地测量与地球动力学, 2012, 32(3): 27~30. http://www.cnki.com.cn/Article/CJFDTOTAL-DKXB201203006.htm CHEN Changyun, REN Jinwei, MENG Guojie, et al. Analysis of modern activity of major faults in northeast margin of Baryan-Har block[J]. Journal of Geodesy and Geodynamics, 2012, 32(3): 27~30. http://www.cnki.com.cn/Article/CJFDTOTAL-DKXB201203006.htm
[11]	周荣军, 闻学泽, 蔡长星, 等.甘孜-玉树断裂带的近代地震与未来地震趋势估计[J].地震地质, 1997, 19(2): 115~124. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ702.002.htm ZHOU Rongjun, WEN Xueze, Cai Changxing, et al. Recent earthquakes and assessment of seismic tendency on the Ganzi-Yushu fault zone[J]. Seismology and Geology, 1997, 19(2): 115~124. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ702.002.htm
[12]	陈杰, 陈宇坤, 丁国瑜, 等. 2001年昆仑山口西8.1级地震地表破裂带[J].第四纪研究, 2003, 23(6): 629~639. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200306005.htm CHEN Jie, CHEN Yukun, DING Guoyu, et al. Surface rupture zones of the 2001 earthquake M_s8.1 West of Kunlun pass, northern Qinghai-Xizang Plateau[J]. Quaternary Sciences, 2003, 23(6): 629~639. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200306005.htm
[13]	徐锡伟, 陈文彬, 于贵华, 等. 2001年11月14日昆仑山库赛湖地震(M_S8.1) 地表破裂带的基本特征[J].地震地质, 2002, 24(1): 1~13. XU Xiwei, CHEN Wenbin, YU Guihua, et al. Characteristic features of the surface ruptures of the Hoh Sai Hu (Kunlunshan) earthquake (M_s8.1), northern Tibetan Plateau, China[J]. Seismology and Geology, 2002, 24(1): 1~13.
[14]	戚帮申, 张鹏, 丰成君, 等.川甘陕交汇地区现今地应力环境与地震危险性[J].中国地质, 2016, 43(5): 1814~1827. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201605029.htm QI Bangshen, ZHANG Peng, FENG Chengjun, et al. Current in-situ stress state and seismic risk in Sichuan-Gansu-Shaanxi border area[J]. Geology in China, 2016, 43(5): 1814~1827. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201605029.htm
[15]	闻学泽.四川西部鲜水河—安宁河—则木河断裂带的地震破裂分段特征[J].地震地质, 2000, 22(3): 239~249. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200003004.htm WEN Xueze. Character of rupture segmentation of the Xianshuihe-Anninghe-Zemuhe fault zone, western Sichuan[J]. Seismology and Geology, 2000, 22(3): 239~249. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200003004.htm