白龙江断裂西段晚第四纪构造活动特征研究

黄雄南; 杨晓平; 胡宗凯; 杨海波

doi:10.11899/zzfy20230405

白龙江断裂西段晚第四纪构造活动特征研究

doi: 10.11899/zzfy20230405

中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029

基金项目: 阿坝州（含盆地地区）1∶25万活断层普查项目（044S20190005）

详细信息

作者简介:
黄雄南，男，生于1974年。博士，副研究员。主要从事构造地质和地震地质研究工作。E-mail：xiongnan_h@sohu.com

12 甘肃省地质局第一区域地质测量队，1973a. 中华人民共和国地质图（1︰200000）碌曲幅. 甘肃省地质局第一区域地质测量队，1973b. 中华人民共和国地质图（1︰200000）卓尼幅.
计量
- 文章访问数: 90
- HTML全文浏览量: 77
- PDF下载量: 40
- 被引次数: 0
出版历程
- 收稿日期: 2023-09-04
- 刊出日期: 2023-12-01

Characteristics of the Late-quaternary Activity of the Western Segment of Bailongjiang Fault

State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China

摘要

摘要: 白龙江断裂位于青藏高原东缘，东昆仑断裂的北侧。白龙江断裂西段的展布及其活动性对研究东昆仑断裂速率向东衰减的机制有重要科学意义。本文根据遥感解译、地质地貌调查、探槽和地质剖面研究白龙江断裂西段的几何展布和断层活动性。白龙江断裂西段分为3 支，包括郎木寺断裂、阿米塘断裂和热尔-旺藏断裂组成的中支、崩巴村断裂构成的南支和下山-迭部断裂构成的北支。这些断裂皆为左旋走滑断层，其中下山-迭部断裂、郎木寺断裂和热尔-旺藏断裂为全新世断层，崩巴村断裂为晚更新世断层。白龙江断裂西段沿袭了前第四纪断裂展布，其分支的几何形态上属于一种典型的尾端构造样式：同向分支断层。研究结果表明白龙江断裂地表上未与东昆仑断裂直接相接，而在深部与之相接，可能分解吸收了东昆仑断裂的部分滑动速率，使得塔藏断裂的滑动速率低于其西侧的玛曲断裂。
- 白龙江断裂 /
- 东昆仑断裂 /
- 晚第四纪 /
- 左旋走滑 /
- 同向分支断层
Abstract: Bailongjiang fault lies parallel and north to the Eastern Kunlun fault in east margin of the Qinghai-Xizang Plateau. The geometry, location and activity of the western segment of the Bailongjiang fault are crucial to understanding the falling slip rate gradient of the eastern Kunlun fault. Three branch faults were found at the western end of the Bailongjiang Faults, including the Central fault, the Southern fault and the Northern fault, revealed by our remote-sensing, field survey and trenching. The Central fault is composed by three segments, the Langmusi fault, the Amitang fault and the Reer-Wanzang fault from the west to the east. The Southern fault and Northern fault are named as the Bengbacun fault and Xiashan-Diebu fault respectively. These faults were active left-lateral strike-slip faults in the late quaternary. The Langmusi fault, the Reer-Wanzang fault and the Xiashan-Diebu fault were active in the Holocene, the Bengbacun fault was active in the late-Pleistocene, and the Amitang fault was supposed to be active from the middle-Pleistocene to late-Pleistocene. In the late quanternary, the activities of the Bailongjiang fault at its western end occurred partially along the pre-Quaternary faults. The geometries of the branch faults show a pattern of the Synthetic branch faults, a typical tip geometry for strike-slip faults. They link forming splay as shear fractures, with the same sense of slip as the master fault. Our results demonstrate the Bailongjiang fault doesn’t connect to the Eastern Kunlun fault on the surface, but is combined with it in deep level. This pattern of faults connection suggests partial slip rate of the Eastern Kunlun fault was absorbed by the Bailongjiang fault in the north, causing the slip rate of the Tazang fault lower than the Maqu fault in the west.
- Bailongjiang fault /
- Eastern Kunlun fault /
- Late quaternary /
- Left-lateral slip /
- Synthetic branch faults
注释:

1) 12 甘肃省地质局第一区域地质测量队，1973a. 中华人民共和国地质图（1︰200000）碌曲幅. 甘肃省地质局第一区域地质测量队，1973b. 中华人民共和国地质图（1︰200000）卓尼幅.

HTML全文

图 1 青藏高原东缘晚第四纪活动断裂分布

Figure 1. Distribution of main active faults of the eastern Qinghai-Xizang Plateau

下载: 全尺寸图片幻灯片

图 2 白龙江断裂西段地质构造与地貌特征

Figure 2. Structural and geomorphological characteristics of the western segment of Bailingjiang fault

下载: 全尺寸图片幻灯片

图 3 郎木寺断裂断错地貌证据

Figure 3. Geomorphic evidences of the Langmusi fault

下载: 全尺寸图片幻灯片

图 4 红星镇东313省道拐弯处郎木寺断裂剖面

Figure 4. Profile of the Langmusi fault in the eastern Hongxing town

下载: 全尺寸图片幻灯片

图 5 郎木寺断裂点R20-22断错地貌与探槽剖面

Figure 5. Faulted topography and trench profile of the Langmusi fault at the field point R20-22

下载: 全尺寸图片幻灯片

图 6 阿米塘断裂断错地貌卫星影像解译

Figure 6. Satellite photographs and faulted topography explanation of the Amitang fault

下载: 全尺寸图片幻灯片

图 7 热尔-旺藏断裂断错地貌

Figure 7. Geomorphic evidences of the Reer-Wangzang fault

下载: 全尺寸图片幻灯片

图 8 热尔-旺藏断裂点R20-94断错地貌解译、露头照片与地质剖面

Figure 8. Faulted linear topography explanation of satellite photography, photographs and structural profile of the fault outcrop at the field point R20-94, the Reer-Wangzang fault

下载: 全尺寸图片幻灯片

图 9 崩巴村断裂断错地质地貌证据

Figure 9. Geomorphic evidences and fault outcrops of the Bengbacun fault

下载: 全尺寸图片幻灯片

图 10 下山-迭部断裂点R20-109和R18断错地貌解译与露头照片

Figure 10. Geomorphic evidences and fault outcrops of the Xiashan-Diebu fault at the field points of R20-109 and R18

下载: 全尺寸图片幻灯片

图 11 下山-迭部断裂点R20-63和R20-73断错地貌解译与露头照片

Figure 11. Linear topography explanation of satellite photography and field photographs of the Xiashan-Diebu fault at the field points of R20-63 and R20-73

下载: 全尺寸图片幻灯片

图 12 下山-迭部断裂点R20-80和R20-87断错地貌解译与露头照片

Figure 12. Linear topography explanation of satellite photography，field photographs and the fault outcrop of the Xiashan-Diebu fault at the field points of R20-80 and R20-87

下载: 全尺寸图片幻灯片

图 13 东昆仑断裂东段（玛沁段至塔藏段）滑动速率向东递减模式

Figure 13. Tectonic model to the falling slip rate gradient of the eastern Kunlun fault （From the Maqin segment to the Tazang segment）

下载: 全尺寸图片幻灯片

参考文献(54)

陈洪凯, 李吉均, 1997. 白龙江流域第四纪以来地貌发育基本模式研究. 重庆交通学院学报, 16（1）: 15—20

Chen H. K. , Li J. J. , 1997. General approach on geomorphologic evolution in Bailongjiang Basin since Quaternary. Journal of Chongqing Jiaotong Institute, 16(1): 15—20. (in Chinese)

崔之久, 高全洲, 刘耕年等, 1996a. 夷平面、古岩溶与青藏高原隆升. 中国科学（D辑）, 26（4）: 378—386.

Cui Z. J., Gao Q. Z., Liu G. N., et al., 1996a. Planation surfaces, palaeokarst and uplift of Xizang (Tibet) Plateau. Science in China Series D-Earth Sciences, 39(4): 391—400.

崔之久, 高全洲, 刘耕年等, 1996b. 青藏高原夷平面与岩溶时代及其起始高度. 科学通报, 41（15）: 1402—1406.

Cui Z. J., Gao Q. Z., Liu G. N., et al., 1997. The initial elevation of palaeokarst and planation surfaces on Tibet Plateau. Chinese Science Bulletin, 42(11): 934—939.

邓起东, 2007. 中国活动构造图（1: 400万）. 北京: 地震出版社.

Deng Q. D., 2007. Map of active tectonics in China. Beijing: Seismological Press. (in Chinese)

杜建军, 马寅生, 尹成明等, 2013. 龙门山北部陕甘川交界三角构造区断裂活动特征研究. 地震学报, 35（4）: 520—533 doi: 10.3969/j.issn.0253-3782.2013.04.007

Du J. J, Ma Y. S. , Yin C. M. , et al. , 2013. Activity characteristics of faults in the triangle structure area in northern part of Longmenshan in the Shaanxi-Gansu-Sichuan junction. Acta Seismologica Sinica, 35(4): 520—533. (in Chinese) doi: 10.3969/j.issn.0253-3782.2013.04.007

付俊东, 任金卫, 张军龙等, 2011. 东昆仑断裂东段下热尔断裂活动特征初步研究. 中国地震, 27（3）: 248—259 doi: 10.3969/j.issn.1001-4683.2011.03.004

Fu J. D. , Ren J. W. , Zhang J. L. , et al. , 2011. A preliminary study on the Xiareer fault of the east Kunlun active fault. Earthquake Research in China, 27(3): 248—259. (in Chinese) doi: 10.3969/j.issn.1001-4683.2011.03.004

高锐, 马永生, 李秋生等, 2006. 松潘地块与西秦岭造山带下地壳的性质和关系——深地震反射剖面的揭露. 地质通报, 25（12）: 1361—1367

Gao R. , Ma Y. S. , Li Q. S. , et al. , 2006. Structure of the lower crust beneath the Songpan block and west Qinling orogen and their relation as revealed by deep seismic reflection profiling. Geological Bulletin of China, 25(12): 1361—1367. (in Chinese)

顾功叙, 1983. 中国地震目录（公元前1831年—公元1969年）. 北京: 科学出版社.

Gu G. X., 1983. Catalogue of Chinese earthquakes. Beijing: Science Press. (in Chinese)

国家地震局震害防御司, 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.

何文贵, 袁道阳, 熊振等, 2006. 东昆仑断裂带东段玛曲断裂新活动特征及全新世滑动速率研究. 地震, 26（4）: 67—75 doi: 10.3969/j.issn.1000-3274.2006.04.010

He W. G. , Yuan D. Y. , Xiong Z. , et al. , 2006. Study on characteristics of new activity and Holocene slip rate along Maqu fault of east Kunlun active fault. Earthquake, 26(4): 67—75. (in Chinese) doi: 10.3969/j.issn.1000-3274.2006.04.010

何玉林, 2013. 青藏高原东缘主干断裂活动性及其构造变形模式研究. 成都: 成都理工大学.

He Y. L., 2013. Study on the main fault activities and tectonic deformation tectonics in the eastern margin of the Qinghai-Tibet Plateau. Chengdu: Chengdu University of Technology. (in Chinese)

胡朝忠, 任金卫, 杨攀新等, 2017. 东昆仑断裂东端塔藏断裂压剪活动与高原隆升作用讨论. 地质学报, 91（7）: 1401—1415 doi: 10.3969/j.issn.0001-5717.2017.07.001

Hu C. Z. , Ren J. W. , Yang P. X. , et al. , 2017. Discussion on the compression-shear activity of the Tazang fault in east Kunlun and uplift of plateau. Acta Geologica Sinica, 91(7): 1401—1415. (in Chinese) doi: 10.3969/j.issn.0001-5717.2017.07.001

李陈侠, 2009. 东昆仑断裂带东段（玛沁—玛曲）晚第四纪长期滑动习性研究. 北京: 中国地震局地质研究所.

Li C. X., 2009. The long-term faulting behavior of the eastern segment （Maqin-Maqu） of the east Kunlun fault since the Late Quaternary. Beijing: Institute of Geology, China Earthquake Administration. (in Chinese)

李陈侠, 徐锡伟, 闻学泽等, 2011. 东昆仑断裂带中东部地震破裂分段性与走滑运动分解作用. 中国科学: 地球科学, 41（9）: 1295—1310.

Li C. X., Xu X. W., Wen X. Z., et al., 2011. Rupture segmentation and slip partitioning of the mid-eastern part of the Kunlun fault, north Tibetan Plateau. Science China Earth Sciences, 54(11): 1730—1745.

李陈侠, 袁道阳, 杨虎等, 2016. 东昆仑断裂带东段分支断裂——阿万仓断裂晚第四纪构造活动特征. 地震地质, 38（1）: 44—64

Li C. X. , Yuan D. Y. , Yang H. , et al. , 2016. The tectonic activity characteristics of Awancang fault in the Late Quaternary, the sub-strand of the eastern Kunlun fault. Seismology and Geology, 38(1): 44—64. (in Chinese)

李峰, 刘华国, 贾启超等, 2018. 青藏高原东缘岷江断裂北段全新世活动特征. 地震地质, 40（1）: 97—106 doi: 10.3969/j.issn.0253-4967.2018.01.008

Li F. , Liu H. G. , Jia Q. C. , et al. , 2018. Holocene active characteristics of the northern segment of the Minjiang fault in the eastern margin of the Tibetan Plateau. Seismology and Geology, 40(1): 97—106. (in Chinese) doi: 10.3969/j.issn.0253-4967.2018.01.008

李昭, 付碧宏, 2022. 东昆仑断裂带玛沁—玛曲段晚第四纪构造活动特征的地貌响应定量研究. 地震地质, 44（6）: 1421—1447

Li Z. , Fu B. H. , 2022. Quantitative analyses of geomorphologic features in response to Late Quaternary tectonic activities along the Maqin-Maqu segment, east Kunlun fault zone. Seismology and Geology, 44(6): 1421—1447. (in Chinese)

梁学战, 陈洪凯, 唐红梅, 2010. 青藏高原东部边缘地区第四纪泥石流发育特性研究. 重庆交通大学学报（自然科学版）, 29（6）: 978—983

Liang X. Z. , Chen H. K. , Tang H. M. , 2010. Studies on debris flow development properties in Quaternary on the eastern edge of Qinghai-Tibet Plateau. Journal of Chongqing Jiaotong University (Natural Science), 29(6): 978—983. (in Chinese)

林茂炳, 苟宗海, 王国芝等, 1996. 四川龙门山造山带造山模式研究. 成都: 成都科技大学出版社.

刘华国, 李峰, 张效亮等, 2018. 青藏高原东缘虎牙断裂晚第四纪活动特征. 地震研究, 41（4）: 594—605

Liu H. G. , Li F. , Zhang X. L. , et al. , 2018. Late Quaternary activity of Huya fault on the eastern margin of the Tibetan Plateau. Journal of Seismological Research, 41(4): 594—605. (in Chinese)

刘树根, 1993. 龙门山冲断带与川西前陆盆地的形成演化. 成都: 成都科技大学出版社.

Liu S. G., 1993. The formation and evolution of Longmenshan thrust zone and western Sichuan foreland basin, Sichuan, China. Chengdu: Press of Chengdu University of Science and Technology. (in Chinese)

刘兴旺, 袁道阳, 邵延秀等, 2015. 甘肃迭部—白龙江南支断裂中东段晚第四纪构造活动特征. 地球科学与环境学报, 37（6）: 111—119

Liu X. W. , Yuan D. Y. , Shao Y. X. , et al. , 2015. Characteristics of Late Quaternary tectonic activity in the middle-eastern segment of the southern branch of Diebu-Bailongjiang fault, Gansu. Journal of Earth Sciences and Environment, 37(6): 111—119. (in Chinese)

任俊杰, 2013. 龙日坝断裂带晚第四纪活动及与其周边断裂的运动学关系. 北京: 中国地震局地质研究所.

Ren J. J., 2013. Late Quaternary activity of the Longriba fault zone and its kinematic relations with adjacent faults. Beijing: Institute of Geology, China Earthquake Administration. (in Chinese)

任俊杰, 徐锡伟, 张世民等, 2017. 东昆仑断裂带东端的构造转换与2017年九寨沟M_S7.0地震孕震机制. 地球物理学报, 60（10）: 4027—4045

Ren J. J. , Xu X. W. , Zhang S. M. , et al. , 2017. Tectonic transformation at the eastern termination of the eastern Kunlun fault zone and seismogenic mechanism of the 8 August 2017 Jiuzhaigou M_S7.0 earthquake. Chinese Journal of Geophysics, 60(10): 4027—4045. (in Chinese)

任俊杰, 吕延武, 丁锐等, 2018. 龙日坝活动断裂带分布图（1∶50000）说明书. 北京: 地震出版社.

邵延秀, 袁道阳, 何文贵等, 2014. 陇南市活断层地震危险性评估. 地震工程学报, 36（3）: 645—655

Shao Y. X. , Yuan D. Y. , He W. G. , et al. , 2014. Seismic hazard assessment for active faults of Longnan City. China Earthquake Engineering Journal, 36(3): 645—655. (in Chinese)

孙翔宇, 詹艳, 赵凌强等, 2020. 东昆仑断裂带东端和2017年九寨沟7.0级地震区深部电性结构探测. 地震地质, 42（1）: 182—197

Sun X. Y. , Zhan Y. , Zhao L. Q. , et al. , 2020. Electrical structure of the 2017 M_S7.0 Jiuzhaigou earthquake region and the eastern terminus of the east Kunlun fault. Seismology and Geology, 42(1): 182—197. (in Chinese)

王海燕, 高锐, 马永生等, 2007. 若尔盖与西秦岭地震反射岩石圈结构和盆山耦合. 地球物理学报, 50（2）: 472—481

Wang H. Y. , Gao R. , Ma Y. S. , et al. , 2007. Basin-range coupling and lithosphere structure between the Zoige and the west Qinling. Chinese Journal of Geophysics, 50(2): 472—481. (in Chinese)

王海燕, 高锐, 李秋生等, 2014. 青藏高原松潘—西秦岭—临夏盆地深地震反射剖面——采集、处理与初步解释. 地球物理学报, 57（5）: 1451—1461

Wang H. Y. , Gao R. , Li Q. S. , et al. , 2014. Deep seismic reflection profiling in the Songpan-west Qinling-Linxia Basin of the Qinghai-Tibet Plateau: data acquisition, data processing and preliminary interpretations. Chinese Journal of Geophysics, 57(5): 1451—1461. (in Chinese)

吴珍汉, 叶培盛, 赵文津等, 2007. 东昆仑南部晚新生代逆冲推覆构造系统. 地质通报, 26（4）: 448—456

Wu Z. H. , Ye P. S. , Zhao W. J. , et al. , 2007. Late Cenozoic overthrust system in the southern east Kunlun Mountains, China. Geological Bulletin of China, 26(4): 448—456. (in Chinese)

许志琴, 侯立玮, 王宗秀, 1992. 中国松潘-甘孜造山带的造山过程. 北京: 地质出版社.

Xu Z. Q., Hou L. W., Wang Z. X., 1992. Orogenic processes of the Songpan-Ganzê orogenic belt of China. Beijing: Geological Publishing House. (in Chinese)

许志琴, 李海兵, 唐哲民等, 2011. 大型走滑断裂对青藏高原地体构架的改造. 岩石学报, 27（11）: 3157—3170

Xu Z. Q. , Li H. B. , Tang Z. M. , et al. , 2011. The transformation of the terrain structures of the Tibet Plateau through large-scale strike-slip faults. Acta Petrologica Sinica, 27(11): 3157—3170. (in Chinese)

俞晶星, 郑文俊, 袁道阳等, 2012. 西秦岭西段光盖山-迭山断裂带坪定-化马断裂的新活动性与滑动速率. 第四纪研究, 32（5）: 957—967

Yu J. X. , Zheng W. J. , Yuan D. Y. , et al. , 2012. Late Quaternary active characteristics and slip-rate of Pingding-Huama fault, the eastern segment of Guanggaishan-Dieshan fault zone (west Qinling Mountain). Quaternary Sciences, 32(5): 957—967. (in Chinese)

袁道阳, 张培震, 刘百篪等, 2004. 青藏高原东北缘晚第四纪活动构造的几何图像与构造转换. 地质学报, 78（2）: 270—278

Yuan D. Y. , Zhang P. Z. , Liu B. C. , et al. , 2004. Geometrical imagery and tectonic transformation of Late Quaternary active tectonics in northeastern margin of Qinghai-Xizang Plateau. Acta Geologica Sinica, 78(2): 270—278. (in Chinese)

袁道阳, 雷中生, 何文贵等, 2007. 公元前186年甘肃武都地震考证与发震构造探讨. 地震学报, 29（6）: 654—663

Yuan D. Y., Lei Z. S., He W. G., et al., 2007. Textual research of Wudu earthquake in 186 B. C. in Gansu Province, China and discussion on its causative structure. Acta Seismologica Sinica, 29(6): 654—663. (in Chinese)

袁道阳, 张波, 王爱国等, 2019. 光盖山-迭山南麓活动断层（1: 50000）说明书. 北京: 地震出版社.

张波, 2020. 西秦岭NWW向断裂系的几何图像与变形分配. 北京: 中国地震局地质研究所.

Zhang B., 2020. Fault geometry and deformation partition of WNW-trending faults in the west Qinling Mountain. Beijing: Institute of Geology, China Earthquake Administration. (in Chinese)

张波, 田勤俭, 朱俊文等, 2022. 西秦岭南部地形异常隆起与构造解释——兼论东昆仑断裂东段的走滑转换. 第四纪研究, 42（3）: 704—716 doi: 10.11928/j.issn.1001-7410.2022.03.07

Zhang B. , Tian Q. J. , Zhu J. W. , et al. , 2022. The topographical uplift of the southern part of the west Qinling Mountains and its tectonic interpretation: a discussion on the strike-slip transition at the eastern end of the east Kunlun fault. Quaternary Sciences, 42(3): 704—716. (in Chinese) doi: 10.11928/j.issn.1001-7410.2022.03.07

张国伟, 郭安林, 姚安平, 2004. 中国大陆构造中的西秦岭-松潘大陆构造结. 地学前缘, 11（3）: 23—32

Zhang G. W., Guo A. L., Yao A. P., 2004. Western Qinling-Songpan continental tectonic node in China's continental tectonics. Earth Science Frontiers 11(3): 23—32. (in Chinese)

张军龙, 2013. 巴颜喀拉地块东北端第四纪隆升量研究. 北京: 中国地震局地质研究所.

Zhang J. L., 2013. The uplift in the northeastern margin of the Bayan Har block since the Quaternary. Beijing: Institute of Geology, China Earthquake Administration. (in Chinese)

张岳桥, 马寅生, 杨农等, 2005. 西秦岭地区东昆仑-秦岭断裂系晚新生代左旋走滑历史及其向东扩展. 地球学报, 26（1）: 1—8

Zhang Y. Q. , Ma Y. S. , Yang N. , et al. , 2005. Late Cenozoic left-slip faulting process of the east Kunlun-Qinling fault system in west Qinling region and its eastward propagation. Acta Geoscientica Sinica, 26(1): 1—8. (in Chinese)

赵志中, 王书兵, 乔彦松等, 2009. 青藏高原东缘晚新生代地质与环境. 北京: 地质出版社.

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, M_S≥4.7）. 北京: 中国科学技术出版社.

Arne D. , Worley B. , Wilson C. , et al. , 1997. Differential exhumation in response to episodic thrusting along the eastern margin of the Tibetan Plateau. Tectonophysics, 280(3—4): 239—256. doi: 10.1016/S0040-1951(97)00040-1

Burchfiel B. C. , Chen Z. L. , Liu Y. , et al. , 1995. Tectonics of the Longmen Shan and adjacent regions, central China. International Geology Review, 37(8): 661—735. doi: 10.1080/00206819509465424

Burchfiel B. C. , Royden L. H. , van der Hilst R. , et al. , 2008. A geological and geophysical context for the Wenchuan earthquake of 12 May 2008, Sichuan, People’s Republic of China. GSA Today, 18(7): 4—11. doi: 10.1130/GSATG18A.1

Kim Y. S. , Sanderson D. J. , 2006. Structural similarity and variety at the tips in a wide range of strike–slip faults: a review. Terra Nova, 18(5): 330—344. doi: 10.1111/j.1365-3121.2006.00697.x

Kirby E. , Harkins N. , Wang E. Q. , et al. , 2007. Slip rate gradients along the eastern Kunlun fault. Tectonics, 26(2): TC2010.

Kirby E. , Harkins N. , 2013. Distributed deformation around the eastern tip of the Kunlun fault. International Journal of Earth Sciences, 102(7): 1759—1772. doi: 10.1007/s00531-013-0872-x

Li H. L. , Zhang Y. Q. , Dong S. W. , et al. , 2020. Neotectonics of the Bailongjiang and Hanan faults: new insights into Late Cenozoic deformation along the eastern margin of the Tibetan Plateau. GSA Bulletin, 132 (9—10): 1845—1862. doi: 10.1130/B35374.1

Ren J. J. , Xu X. W. , Yeats R. S. , et al. , 2013. Millennial slip rates of the Tazang fault, the eastern termination of Kunlun fault: implications for strain partitioning in eastern Tibet. Tectonophysics, 608: 1180—1200. doi: 10.1016/j.tecto.2013.06.026

Van Der Woerd J. , Tapponnier P. , Ryerson F. J. , et al. , 2002. Uniform postglacial slip-rate along the central 600 km of the Kunlun fault (Tibet), from ²⁶Al, ¹⁰Be, and ¹⁴C dating of riser offsets, and climatic origin of the regional morphology. Geophysical Journal International, 148(3): 356—388. doi: 10.1046/j.1365-246x.2002.01556.x

Xu Z. Q. , Ji S. C. , Li H. B. , et al. , 2008. Uplift of the Longmen Shan range and the Wenchuan earthquake. Episodes, 31(3): 291—301. doi: 10.18814/epiiugs/2008/v31i3/002

Zhang B. , Wang A. G. , Yuan D. Y. , et al, 2021. Slip rates and paleoearthquakes along the east segment of the Guanggaishan–Dieshan fault zone, west Qinling Range, NW China. International Journal of Earth Sciences, 110(1): 213—232. doi: 10.1007/s00531-020-01947-0

施引文献

资源附件(0)

访问统计