龙门山构造带南段向西南延伸的遥感影像证据及地震地质意义

马晓雪; 吴中海; 李家存; 周春景; 李凯; 王继龙

龙门山构造带南段向西南延伸的遥感影像证据及地震地质意义

马晓雪^{1, 2, 3, 4,},
吴中海^{2, 4, ,},
李家存^{1, 3},
周春景^{2, 4},
李凯^{1, 2, 3, 4},
王继龙^{2, 4, 5}

1.
首都师范大学资源环境与旅游学院, 北京 100048
2.
中国地质科学院地质力学研究所, 北京 100081
3.
资源环境与地理信息系统北京市重点实验室, 北京 100048
4.
国土资源部新构造运动与地质灾害重点实验室, 北京 100081
5.
中国地质大学地球科学与资源学院, 北京 100083

基金项目:

中国地质调查局地质调查项目 12120114002101

中国地质调查局地质调查项目 DD20160268

国家自然科学基金项目 41571013

国家自然科学基金项目 41171009

详细信息

作者简介:
马晓雪(1991-), 女, 硕士研究生, 主要从事3S技术与地学应用研究。E-mail:mxx120591@sina.com

通讯作者:
吴中海(1974-), 男, 博士, 研究员, 主要从事新构造和活动构造研究。E-mail:wzhh4488@sina.com

中图分类号: P627;P315.2
计量
- 文章访问数: 312
- HTML全文浏览量: 83
- PDF下载量: 31
- 被引次数: 0
出版历程
- 收稿日期: 2016-03-25
- 刊出日期: 2016-09-01

REMOTE SENSING EVIDENCE OF THE SOUTH SEGMENT OF LONGMENSHAN FAULT ZONE EXTENDING TO SOUTHWEST AND ITS SEISMIC GEOLOGICAL SIGNIFICANCE

MA Xiao-xue^{1, 2, 3, 4
,},
WU Zhong-hai^{2, 4
, ,},
LI Jia-cun^{1, 3},
ZHOU Chun-jing^{2, 4},
LI Kai^{1, 2, 3, 4},
WANG Ji-long^{2, 4, 5}

1.
College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
Beijing Key Laboratory of Resource Environment and Geographic Information System, Beijing 100048, China
4.
Key Laboratory of Neotectonic Movement and Geohazard, Ministry of Land and Resources, Beijing 100081, China
5.
College of Earth Science and Resources, China University of Geosciences, Beijing 100083, China

摘要

摘要: 在系统总结活动断裂遥感影像解译标志的基础上，利用Landsat ETM、Google Earth及ASTER GDEM等影像资料，结合前人研究成果，重点分析了龙门山构造带南段主要活动断裂的空间展布及几何学与运动学特征。研究结果表明，龙门山构造带在向南延伸过程中发生了明显的断裂分散现象，整个断裂带逐渐展宽，主要包括5条断裂带且其中包含多条次级断裂，至最南端被北西向鲜水河左旋走滑断裂带阻挡。其中活动性较为明显的断裂自西向东主要有4条：泸定断裂、天全断裂、芦山断裂和大邑-名山断裂，前两者是北川-映秀断裂的南延分支，而后两者是安县-灌县断裂的南延部分。由于龙门山构造带南段的构造变形被分解至多条次级断裂上，导致单条断裂错断地表的活动迹象明显变弱，因此单条断裂的潜在发震频率和强度也将相应变小，但潜在震源区会更为分散。结合已有的地震地质资料认为，未来应注意泸定和雅安2个地区的地壳稳定性及未来强震危险性问题。
- 龙门山构造带 /
- 遥感解译 /
- 活动断裂 /
- 潜在震源区 /
- 芦山地震
Abstract: Combining remote sensing imagery interpretation of active faults with Landsat ETM, Google Earth and ASTER GDEM image data, this paper analysed the spatial distribution and geometry and motion characteristics of the south section of Longmenshan tectonic belt. The results showed that Longmenshan tectonic belt occurred obvious fracture dispersion in the process of extending to the south. The tectonic zone gradually widened, developing 5 faults and many secondary faults. The southernmost of Longmenshan tectonic zone was stopped by Xianshuihe sinistral strike-slip fault. Activities of Luding fault, Tianquan fault, Lushan fault and Dayi-Mingshan fault are more obvious. The former two are south-extending branches of Beichuan-Yingxiu fault, the latter two are south-extending branches of Anxian-Guanxian fault. The tectonic deformation of south Longmenshan tectonic belt was dispersed to a plurality of secondary faults, resulting in surface activity signs of single fault weaken significantly. So the potential earthquake frequency and intensity of single fault will also be correspondingly smaller, but potential seismic source region will be more dispersed. According to the existing seismic geological data, we should pay attention to the crustal stability and strong earthquake risk in Ya'an and Luding areas in the future.
- Longmenshan tectonic belt /
- remote sensing interpretation /
- active fault /
- potential seismic source region /
- Lushan earthquake

HTML全文

图 1 龙门山断裂带及邻区地质简图和地层剖面^[26]

Pc-前寒武系; Z-新元古系(震旦系); Pz-古生界; T-三叠系; J-侏罗系; K-白垩系; E-始新统; 红线为新生代断裂

Figure 1. Simplified geologic map and stratigraphic profiles of the Longmenshan fault zone and its adjacent region

下载: 全尺寸图片幻灯片

图 2 龙门山断裂带南段地震烈度图

(数据来源：中国地震信息网http://www.csi.ac.cn/publish/main/837/1074/index.html)

Figure 2. Earthquake intensity map of the southern segment of Longmenshan fault zone

下载: 全尺寸图片幻灯片

图 3 龙门山断裂带南段活动断裂研究现状与地震分布图(ASTER GDEM)^[27~30]

Figure 3. Active faults and earthquakes in the southern segment of Longmenshan fault zone (ASTER GDEM)

下载: 全尺寸图片幻灯片

图 4 龙门山断裂带南段几何展布及地震分布图(ETM7)

Figure 4. Geometric distribution of the south segment of Longmenshan fault zone and earthquake distribution(ETM7)

下载: 全尺寸图片幻灯片

图 5 卧龙—硗碛断裂带几何展布及错断地貌特征

Figure 5. Geometric distribution of Wolong-Yaoji fault zone and and features of displacing landforms

下载: 全尺寸图片幻灯片

图 6 泸定断裂带的几何展布及错断地貌特征

Figure 6. Geometric distribution of Luding fault zone and features of dislocation landforms

下载: 全尺寸图片幻灯片

图 7 天全断裂带的几何展布及地貌特征

Figure 7. Geometric distribution of Tianguan fault zone and its landform features

下载: 全尺寸图片幻灯片

图 8 芦山断裂和大邑-名山断裂的几何展布及错断地貌特征

Figure 8. Geometric distribution of Lushan and Dayi-Mingshan faults and their dislocation landform features

下载: 全尺寸图片幻灯片

图 9 龙门山断裂带南段主要活动断裂的延伸

Figure 9. Extension of the major active faults in the south segment of Longmenshan fault zone

下载: 全尺寸图片幻灯片

图 10 龙门山断裂带南段的三维结构与芦山7.0地震发震构造示意图

Figure 10. A model map showing the three-dimensional structure of the southern section of LongmenShan fault zone and seismogenic structures associated with the Ms7.0 Lushan earthquake

下载: 全尺寸图片幻灯片

表 1 卧龙-硗碛断裂带主要断裂参数及遥感标志

Table 1. The major activity faults' parameters and remote sensing marks in Wolong-Yaoji fault

断裂带	编号	断裂名称	走向	长度/km	性质	活动性	遥感标志
耿达—陇东断裂带	F1-1	卧龙断裂	NE	78	右旋走滑	弱	断层三角面和雁列状冲沟，冲沟右旋错动
	F1-2	耿达断裂	NNE	26	右旋走滑	极弱	水系向右偏转
	F1-3	硗碛断裂	NEE	35	右旋走滑	极弱	影像特征不明显
	F1-4	城墙岩断裂	E	39	右旋走滑	极弱	断层三角面和雁列状冲沟，冲沟向右偏转
	F1-5	中岗断裂	NE	26	右旋走滑	极弱	影像特征不明显

下载: 导出CSV

表 2 泸定断裂带主要断裂参数及遥感标志

Table 2. The major fault parameters and remote sensing marks in Luding fault zone

编号	断裂名称	走向	长度/km	性质	活动性	遥感标志
F2-1	水磨断裂	NE	35	右旋走滑	中等	断裂沿沟谷延伸，断层陡坎发育
F2-2	三江断裂	NE	24	右旋走滑	极弱	发育一系列断层崖和断层三角面
F2-3	泸定断裂	NE—NNE	168	右旋走滑	中等	大渡河发生明显偏移，偏移量高达4.7±0.5 km，山脊错动
F2-4	宝兴断裂	NE—NEE	49	右旋走滑	中等	西河发生明显偏移，偏移量高达6.4±0.5 km

下载: 导出CSV

表 3 天全断裂带主要断裂参数及遥感标志

Table 3. The major fault parameters and remote sensing marks in Tianguan fault zone

编号	断裂名称	走向	长度/km	性质	活动性	遥感标志
F3-1	天全断裂	NE—NNE	172	右旋走滑	中等	断裂沿线性沟谷展布，断裂谷发育，断裂切割河流谷坡形成断层崖、断层沟槽及垭口
F3-2	飞水断裂	NE	30	右旋走滑	极弱	无明显错断现象，断裂行迹不清晰
F3-3	大川断裂	NNE	30	右旋走滑	极弱	沿断裂发育一排整齐的断裂谷，断裂两侧地貌差异明显
F3-4	双石断裂	NE	21	右旋走滑	极弱	断层崖发育，水系右旋错动
F3-5	永河断裂	NE	28	右旋走滑	极弱	断裂沿线性沟谷发育

下载: 导出CSV

表 4 芦山断裂和大邑-名山断裂的参数及遥感标志

Table 4. The major fault parameters and remote sensing marks in Lushan fault and Dayi-Mingshan fault

编号	断裂名称	走向	长度/km	性质	活动性	遥感标志
F4	芦山断裂	NNE—NE	115	逆冲	中等	断裂两侧地形差异较大，发育雁列状冲沟
F5	大邑—名山断裂	E—N	133	逆冲	中等	断裂沿盆山边界展布，断裂西侧发育一系列断层三角面和小鼓丘

下载: 导出CSV

参考文献(45)

[1]	邓起东, 陈社发.龙门山及其邻区的构造和地震活动及动力学[J].地震地质, 1994(4):389~403. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ404.013.htm DENG Qi-dong, CHEN She-fa.Tectonics, scismisity and dynamics of Longmenshan Mountains and its adjacent regions[J].Seisoloyg and geology, 1994(4):389~403. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ404.013.htm
[2]	闻学泽, 张培震, 杜方, 等. 2008年汶川8.0级地震发生的历史与现今地震活动背景[J].地球物理学报, 2009, 52(2):444~454. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200902017.htm WEN Xue-ze, ZHANG Pei-zhen, DU Fang, et al.The background of historical and modern seismic activities of the occurrence of the 2008 Ms8.0 Wenchuan, Sichuan, earthquake[J]. Chinese Journal of Geophysics, 2009, 52(2):444~454. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX200902017.htm
[3]	徐锡伟, 闻学泽, 韩竹军, 等.四川芦山7.0级强震:一次典型的盲逆断层型地震[J].科学通报, 2013, 58(20):1887~1893. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201320002.htm XU Xi-wei, WEN Xue-ze, HAN Zhu-jun, et al. LushanMs 7.0 earthquake:A blind reserve-fault earthquake[J]. Chinese Science Bulletin, 2013, 58, (20):1887~1893. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201320002.htm
[4]	徐锡伟, 陈桂华, 于贵华, 等.芦山地震发震构造及其与汶川地震关系讨论[J].地学前缘, 2013, 20(3):11~20. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201303002.htm XU Xi-wei, CHEN Gui-hua, YU Gui-hua, et al. Seismogenic structure of Lushan earthquake and its relationship with Wenchuan earthquake[J]. Earth Science Frontiers, 2013, 20(3):11~20. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201303002.htm
[5]	郑文俊, 郭华, 袁道阳, 等.遥感影像信息在活动断裂研究中的应用[J].高原地震, 2002, 14(2):15~21. http://www.cnki.com.cn/Article/CJFDTOTAL-GYDZ200202002.htm ZHENG Wen-jun, GUO Hua, YUAN Dao-yang, et al. Application of remote sensing image information in the research of active faults[J]. Earthquake Research in Plateau, 2002, 14(2):15~21. http://www.cnki.com.cn/Article/CJFDTOTAL-GYDZ200202002.htm
[6]	Molnar P, Tapponnier P. Cenozoic Tectonics of Asia:Effects of a Continental Collision:Features of recent continental tectonics in Asia can be interpreted as results of the India-Eurasia collision[J]. British Journal of Nutrition, 1975, 189(4201):419~426. doi: 10.1007/s12583-010-0009-0
[7]	S. Kaya. Tracing the geometry of an active fault using remote sensing and digital elevation model:Ganos segment, North Anatolian Fault zone, Turkey[J]. International Journal of Remote Sensing, 2004, 25(19):3843~3855. doi: 10.1080/01431160310001652394
[8]	李家存, 吴中海, 张铎, 等.青海玉树地区主要活动断裂的遥感影像解译及构造活动性[J].地质通报, 2014, 33(4):535~550. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201404010.htm LI Jia-cun, WU Zhong-hai, ZHANG Duo, et al. Remote sensing image interpretation and tectonic activity study of the main active faults in Yushu area, Qinghai Province[J]. Geological Bulletin of China, 2014, 33(4):535~550. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201404010.htm
[9]	马丹, 吴中海, 李家存, 等.川西理塘断裂带的空间展布与第四纪左旋走滑活动的遥感影像标志[J].地质学报, 2014, 88(8):1417~1435. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201408005.htm MA Dan, WU Zhong-hai, LI Jia-cun, et al. Geometric distribution and the quaternary activity of Litang Active Fault zone based on remote sensing[J]. Acta Geologica Sinica, 2014, 88(8):1417~1435. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201408005.htm
[10]	谭锡斌, 徐锡伟, 李元希, 等.龙门山中段中央断裂和前山断裂的晚新生代垂向活动性差异及其构造意义[J].地球物理学报, 2015, 58(1):143~152. doi: 10.6038/cjg20150112 TAN Xi-bin, XU Xi-wei, LI Yuan-xi, et al. Differential Late-Cenozoic vertical motions of the Beichuan-Yingxiu Fault and Jiangyou-Guanxian Fault in the central Longmenshan range and their tectonic implications[J]. Chinese Journal of Geophysics, 2015, 58(1):143~152. doi: 10.6038/cjg20150112
[11]	李勇, 周荣军, Densmore A L, 等.青藏高原东缘龙门山晚新生代走滑-逆冲作用的地貌标志[J].第四纪研究, 2006, 26(1):40~51. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601005.htm LI Yong, ZHOU Rong-jun, Desmore A L, et al. Geomorphic evidence for the Late Cenozoic strike-slipping and thrusting in Longmen Mountain at the eastern margin of the Tibetan Plateau[J]. Quaternary Sciences, 2006, 26(1):40~51. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601005.htm
[12]	刘树根, 罗志立, 戴苏兰, 等.龙门山冲断带的隆升和川西前陆盆地的沉降[J].地质学报, 1995, 69(3):204~214. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199503001.htm LIU Shu-gen, LUO Zhi-li, DAI Su-lan, et al. The uplift of the Longmenshan thrust belt and subsidence of the western Sichuan foreland basin[J]. Acta Geologica Sinica, 1995, 69(3):204~214. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199503001.htm
[13]	李勇, 黄润秋, 周荣军, 等.龙门山地震带的地质背景与汶川地震的地表破裂[J].工程地质学报, 2009, 17(1):3~18. http://www.cnki.com.cn/Article/CJFDTOTAL-GCDZ200901003.htm LI Yong, HUANG Run-qiu, ZHOU Rong-jun, et al. Geological background of Longmenshan seismic belt and surface ruptures in Wenchuan earthquake[J]. Journal of Engineering Geology, 2009, 17(1):3~18. http://www.cnki.com.cn/Article/CJFDTOTAL-GCDZ200901003.htm
[14]	李勇, 孙爱珍.龙门山造山带构造地层学研究[J].地层学杂志, 2000, 24(3):201~206. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ200003005.htm LI Yong, SUN Ai-zhen. Tectostratigraphy of LongmenshanOrogen[J]. Journal of Stratigraphy, 2000, 24(3):201~206. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ200003005.htm
[15]	唐荣昌, 立德华.松潘-龙门山地区主要活动断裂带第四纪活动特征[J].中国地震, 1991, (3):64~71. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD199103006.htm TANG Rong-chang, LI De-hua. The quaternary activity characteristics of several major active faults in the Songpan-Longmenshan region[J]. Earthquake Research in China, 1991, (3):64~71. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD199103006.htm
[16]	刘健, 熊探宇, 赵越, 等.龙门山活动断裂带运动学特征及其构造意义[J].吉林大学学报:地球科学版, 2012, 42(S2):320~330. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2012S2034.htm LIU Jian, XIONG Tan-yu, ZHAO Yue, et al. Kinematic characteristics Longmenshan active fault zone and its tectonic implication[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(S2):320~330. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2012S2034.htm
[17]	陈国光, 计凤桔, 周荣军, 等.龙门山断裂带晚第四纪活动性分段的初步研究[J].地震地质, 2007, 29(3):657~673. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200703021.htm CHEN Guo-guang, JI Feng-ju, ZHOU Rong-jun, et al. Primary research of activity segmentation of Longmenshan Fault zone since Late-Quateranary[J]. Seismology and Geology, 2007, 29(3):657~673. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200703021.htm
[18]	李智武, 刘树根, 陈洪德, 等.龙门山冲断带分段-分带性构造格局及其差异变形特征[J].成都理工大学学报:自然科学版, 2008, 35(4):440~454. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200804014.htm LI Zhi-wu, LIU Shu-gen, CHEN Hong-de, et al. Structural segmentation and zonation and differential deformation across and along the Longmen thrust belt, West Sichuan, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2008, 35(4):440~454. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200804014.htm
[19]	England P, Molnar P. Right-lateral shear and rotation as the explanation for strike-slip faulting in eastern Tibet[J]. Nature, 1990(6262):140.
[20]	Jean-Philippe A, Paul T. Kinematic Model of Active Deformation in Central-Asia[J]. Geophysical Research Letters, 1993, 20(10):895~898. doi: 10.1029/93GL00128
[21]	Burchfiel B C, Chen Zhiliang, Liu Yupinc, et al. Tectonics of the Longmenshan and adjacent regions, Central China[J]. International Geology Review, 1995, 37(8):661~735. doi: 10.1080/00206819509465424
[22]	Chen Z, Burchfiel B C, Liu Y, et al. Global Positioning System measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation[J]. Journal of Geophysical Research Solid Earth, 2000, 105(7):16215~16227.
[23]	LI Yong, Densmore A L, Allen P A, et al. Sedimentary responses to thrusting and strike-slipping of Longmen Shan along eastern margin of Tibetan Plateau and their implication of Cimmerian continents and India/Eurasia collision[J]. ScientiaGeologicaSinica, 2001, 10(4):223~243.
[24]	李勇, 周荣军, Densmore, 等.青藏高原东缘龙门山晚新生代走滑挤压作用的沉积响应[J].沉积学报, 2006, 24(2):153~164. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200602000.htm LI Yong, ZHOU Rong-jun, Densmore, et al. Sedimentary responses to Late Cenozoic thrusting and strike slipping of Longmenshan along Eastern margin of Tibetan Plateau[J]. ActaSedimentologicaSinica, 2006, 24(2):153~164. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200602000.htm
[25]	唐文清, 刘宇平, 陈智梁, 等.基于GPS技术的活动断裂监测——以鲜水河、龙门山断裂为例[J].山地学报, 2007, 25(1):103~107. http://www.cnki.com.cn/Article/CJFDTOTAL-SDYA200701011.htm TANG Wen-qing, LIU Yu-ping, CHEN Zhi-liang, et al. Monitoring of faults activity based on GPS[J]. Journal of Mountain Science, 2007, 25(1):103~107. http://www.cnki.com.cn/Article/CJFDTOTAL-SDYA200701011.htm
[26]	Burchfiel B C, Royden L H, Hilst R D V D, et al. A geological and geophysical context for the Wenchuan earthquake of 12 May 2008, Sichuan, People's Republic of China[J]. Gsa Today, 2008, 18(18):4~11. http://www.doc88.com/p-370141786962.html
[27]	邓起东.中国活动构造图(1:400万)[M].北京:地震出版社, 2007. DENG Qi-dong. Chinese active tectonic map (1:4000000)[M]. Beijing:Seismological Press, 2007.
[28]	张岳桥, 李海龙.龙门山断裂带西南段晚第四纪活动性调查与分析[J].第四纪研究, 2010, 30(4):699~710. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201004007.htm ZHANG Yue-qiao, LI Hai-long. Late quaternary active along the SW segment of the Longmenshan fault zone[J]. Quaternary Sciences, 2010, 30(4):699~710. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ201004007.htm
[29]	陈立春, 冉勇康, 王虎, 等.芦山地震与龙门山断裂带南段活动性[J].科学通报, 2013(20):1925~1932. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201320007.htm CHEN Li-chun, RAN Yong-kang, WANG Hu, et al. The Lushan Ms 7.0 earthquake and activity of the southern segment of the Longmenshan fault zone[J]. Chinese Science Bulletin, 2013, (20):1925~1932. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201320007.htm
[30]	国家地震局地震研究所.中国主要活动断裂带卫星图像集[M].北京:科学出版社, 1989:65~67.
[31]	吴中海, 张岳桥, 胡道功.新构造、活动构造与地震地质[J].地质通报, 2014, 33(4):391~402. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201404001.htm WU Zhong-hai, ZHANG Yue-qiao, HU Dao-gong.Neotectonics, active tectonics and earthquake geology[J]. Geological Bulletin of China, 2014, 33(4):391~402. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201404001.htm
[32]	谢广林, 蒋蔺珍, 朱源明, 等.活动断裂的影象标志[J].地震, 1982, (3):23~26. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZN198203008.htm XIE Guang-lin, JIANG Lin-zhen, ZHU Yuan-ming, et al.The image mark of active faults[J]. Earthquake, 1982, (3):23~26. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZN198203008.htm
[33]	蒋蔺珍.活动断裂垂直错动的影象标志[J].华南地震, 1985, (4):12~19. http://www.cnki.com.cn/Article/CJFDTOTAL-HNDI198504001.htm JIANG Lin-zhen.The image mark of the vertical dislocation of active fault[J].South China Journal of Seismology, 1985, (4):12~19. http://www.cnki.com.cn/Article/CJFDTOTAL-HNDI198504001.htm
[34]	丁国瑜.活动走滑断裂带的断错水系与地震[J].地震, 1982, (1):3~8. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZN198201000.htm DING Guo-yu. Faulted river system and earthquake of active strike slip fault zone[J]. Earthquake, 1982, (1):3~8. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZN198201000.htm
[35]	张岳桥, 董树文, 侯春堂, 等.四川芦山2013年Ms7.0地震发震构造初步研究[J].地质学报, 2013, 87(6):747~758. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201306001.htm ZHANG Yue-qiao, DONG Shu-wen, HOU Chun-tang, et al. Preliminary study on the seismotectonics of the 2013 Lushan Ms7.0 earthquake, West Sichuan[J]. ActaGeologicaSinica, 2013, 87(6):747~758. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201306001.htm
[36]	李传友, 徐锡伟, 甘卫军, 等.四川省芦山7.0地震发震构造分析[J].地震地质, 2013, 35(3):671~683. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201303020.htm LI Chuan-you, XU Xi-wei, GAN Wei-jun, et al. Seismogenic structures associated with the 20 April 2013 Ms 7.0 Lushan earthquake, Sichuan province[J]. Seismology and Geology, 2013, 35(3):671~683. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201303020.htm
[37]	李勇, 周荣军, 赵国华, 等.龙门山前缘的芦山地震与逆冲-滑脱褶皱作用[J].成都理工大学学报:自然科学版, 2013, 40(4):353~363. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201304002.htm LI Yong, ZHOU Rong-jun, ZHAO Guo-hua, et al. Thrusting and detachment folding of Lushan earthquake in front of Longmenshan mountains[J]. Journal of Chengdu University of technology, 2013, 40(4):353~363. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201304002.htm
[38]	董绍鹏, 韩竹军, 尹金辉, 等.龙门山山前大邑断裂活动时代与最新构造变形样式初步研究[J].地震地质, 2008, 30(4):996~1003. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200804018.htm
[39]	杨晓平, 邓忠文.龙门山断裂带南段错断晚更新世以来地层的证据[J].地震地质, 1999, 21(4):341~345. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ199904006.htm YANG Xiao-ping, DENG Zhong-wen, et al. The evidence of the south Longmenshan fault zones cutting Late Quaternary stratum[J]. Seismology and Geology, 1999, 21(4):341~345. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ199904006.htm
[40]	唐文清, 陈智梁, 刘宇平, 等.青藏高原东缘鲜水河断裂与龙门山断裂交会区现今的构造活动[J].地质通报, 2005, 24(12):1169~1172. doi: 10.3969/j.issn.1671-2552.2005.12.013 TANG Wen-qing, CHEN Zhi-liang, LIU Yu-ping, et al. Present-day tectonics activity in the intersection area of the Xianshuihe fault and Longmenshan fault on the eastern margin of the Qinghai-Tibet Plateau[J]. Geological Bulletin of China, 2005, 24(12):1169~1172. doi: 10.3969/j.issn.1671-2552.2005.12.013
[41]	刘峡, 孙东颖, 马瑾, 等. GPS结果揭示的龙门山断裂带现今形变与受力——与川滇地区其他断裂带的对比研究[J].地球物理学报, 2014(4):1091~1100. doi: 10.6038/cjg20140407 LIU Xia, SUN Dong-ying, MA Jin, et al. Present-day deformation and stress state of Longmenshan fault from GPS results-comparative research on active faults in Sichuan-Yunnan region[J]. Chinese Journal of Geophysics, 2014(4):1091~1100. doi: 10.6038/cjg20140407
[42]	赵炜喆, 吴忠良, 蒋长胜, 等.用地震资料估计的龙门山断裂深部形变及其对于汶川地震成因的意义[J].地质学报, 2008, 82(12):1778~1787. doi: 10.3321/j.issn:0001-5717.2008.12.013 ZHAO Yi-zhe, WU Zhong-liang, JIANG Chang-sheng, et al. Present deep deformation along the Longmenshanfault by seismic dataand implications for the tectonic context of the Wenchuanearthquake[J]. ActaGeologicaSinica, 2008, 82(12):1778~1787. doi: 10.3321/j.issn:0001-5717.2008.12.013
[43]	石绍先, 曹刻, 和宏伟, 等.川滇地区成组强震活动的基本特征[J].地震研究, 2003, 26(增刊):55~61. http://www.cnki.com.cn/Article/CJFDTOTAL-DZYJ2003S1008.htm SHI Shao-xian, CAO Ke, HE Hong-wei, et al. The basic features of seismicity of grouped strong earthquakes in Sichuan-Yunnan region[J]. Journal of Seismological Research, 2003, 26(Sup.):55~61. http://www.cnki.com.cn/Article/CJFDTOTAL-DZYJ2003S1008.htm
[44]	孟文, 陈群策, 吴满路, 等.龙门山断裂带现今构造应力场特征及分段性研究[J].地球物理学进展, 2013, 28(3):1150~1160. doi: 10.6038/pg20130306 MENG Wen, CHEN Qun-ce, WU Man-lu, et al. Research on segmentation and characteristic of tectonic stress field of Longmenshan fault zone[J]. Progress in Geophys, 2013, 28(3):1150~1160. doi: 10.6038/pg20130306
[45]	安其美, 丁立丰, 王海忠, 等.龙门山断裂带的性质与活动性研究[J].大地测量与地球动力学, 2004, 24(2):115~119. http://www.cnki.com.cn/Article/CJFDTOTAL-DKXB200402020.htm AN Qi-mei, DING Li-feng, WANG Hai-zhong, et al. Research of property and activity of Longmen Mountain fault zone[J]. Journal of Geodesy and Geodynamics, 2004, 24(2):115~119. http://www.cnki.com.cn/Article/CJFDTOTAL-DKXB200402020.htm