SURFACE DEFORMATION CHARACTERISTICS OF THE 2025 DINGRI MW7.1 EARTHQUAKE DERIVED FROM GF-2 IMAGERY USING OPTICAL IMAGE CORRELATION TECHNIQUE

doi:10.3969/j.issn.0253-4967.20250066

SEISMOLOGY AND GEOLOGY ›› 2026, Vol. 48 ›› Issue (4): 1035-1051.DOI: 10.3969/j.issn.0253-4967.20250066

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SURFACE DEFORMATION CHARACTERISTICS OF THE 2025 DINGRI M_W7.1 EARTHQUAKE DERIVED FROM GF-2 IMAGERY USING OPTICAL IMAGE CORRELATION TECHNIQUE

SU Qiang¹⁾(), PAN Jia-wei¹^,²^,³⁾^,^*(), LI Hai-bing¹^,²^,³⁾, LIU Fu-cai¹^,²⁾, Marie-luce Chevalier¹^,²^,³⁾, YANG Shao-hua¹^,²^,³⁾, WU Kun-gang¹^,⁴⁾, JIANG Chen-yi¹⁾

¹⁾ Key Laboratory of Continental Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
²⁾ National Field Observation and Research Station(Jiangsu Donghai) for Continental Deep Hole Crustal Activity, Lianyungang 222300, China
³⁾ State Key Laboratory of Deep Earth and Mineral Exploration, Beijing 100094, China
⁴⁾ Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Received:2025-03-14 Revised:2025-04-27 Online:2026-08-20 Published:2026-09-09

基于GF-2影像相关性匹配的2025年 M_W7.1 西藏定日地震地表变形特征

苏强¹⁾(), 潘家伟¹^,²^,³⁾^,^*(), 李海兵¹^,²^,³⁾, 刘富财¹^,²⁾, Marie-Luce Chevalier¹^,²^,³⁾, 杨少华¹^,²^,³⁾, 吴坤罡¹^,⁴⁾, 江晨轶¹⁾

¹⁾ 中国地质科学院地质研究所, 自然资源部大陆动力学重点实验室, 北京 100037
²⁾ 江苏东海大陆深孔地壳活动国家野外科学观测研究站, 连云港 222300
³⁾ 深地探测与矿产勘查全国重点实验室, 北京 100094
⁴⁾ 中国地质科学院地质力学研究所, 自然资源部活动构造与地质安全重点实验室, 北京 100081

通讯作者: ^* 潘家伟, 男, 1983生, 研究员, 主要从事青藏高原活动构造与地震地质研究, E-mail: jiawei-pan@foxmail.com。
作者简介:
苏强, 男, 2000年生, 现为中国地质科学院地质研究所地质学专业在读硕士研究生, 从事遥感与活动构造相关研究, E-mail: su202309@163.com。
基金资助:
中国地质调查局项目(DD20240100703); 科技基础资源调查专项(2021FY100101); 国家自然科学基金(42372274); 国家自然科学基金(42325207); 中国地质科学院地质力学所基本科研业务项目(DZLXJK202413)

Abstract

Abstract:

Accurate quantification of near-surface coseismic fault-slip distribution is critical for understanding earthquake rupture propagation and fault structural evolution. Traditional field surveys and geodetic methods have inherent limitations in resolving spatially distributed coseismic surface deformation with high precision. In recent years, rapid advances in sub-pixel correlation techniques applied to optical satellite imagery have provided an effective approach for comprehensive and high-resolution quantification of coseismic surface displacements. On 7 January 2025, an M_W7.1 earthquake struck Dingri County, Tibet, at a focal depth of 10km, causing significant casualties and economic losses and generating a coseismic surface rupture zone of approximately 35km along the Dingmu Co Fault. Following the event, numerous studies investigated coseismic surface deformation using high-resolution remote sensing interpretation, field surveys, GNSS, and Interferometric Synthetic Aperture Radar(InSAR). However, owing to methodological limitations, the distributed surface deformation associated with the Dingri earthquake has not yet been fully resolved. To further constrain the coseismic surface deformation characteristics of this event, this study uses pre- and post-event Chinese Gaofen-2 (GF-2) optical satellite images with a spatial resolution of 0.81m. Coseismic displacements are quantitatively derived using sub-pixel image correlation implemented in the COSI-Corr software package.

The image correlation results demonstrate that GF-2 imagery has strong capability for quantifying coseismic displacement and clearly reveals an approximately 6km-long coseismic surface rupture segment northeast of Nixia Co. Consistent with this result, field investigations indicate that the area northeast of Nixia Co experienced the largest coseismic surface rupture, with a maximum vertical offset approaching 3m. The rupture traces extracted from image correlation show good overall agreement with those mapped through field surveys and high-resolution unmanned aerial vehicle(UAV)imagery. The north-south displacement field derived from image correlation indicates northward motion of the eastern footwall and southward motion of the western hanging wall, consistent with field observations of coseismic rupture characteristics. In addition, the coseismic displacement vector field clearly reveals oblique slip, with the western hanging wall moving toward the SWW and the eastern footwall moving toward the NEE. Integrated analysis of multi-source datasets indicates that the Dingri earthquake was dominated by normal faulting with a significant sinistral, or left-lateral, strike-slip component.

Based on the image correlation results, horizontal displacement components in the east-west and north-south directions were extracted along the rupture trace using swath profiles. The results indicate that east-west extensional displacement across the Nixia Co segment predominantly ranges from 0.8 to 2.8m, with an average of approximately 2.0m and a maximum of 3.9m. The sinistral strike-slip displacement mainly ranges from 0.4 to 1.6m, with an average of approximately 0.9m and a maximum of 1.9m. Comparative analysis shows that, although the deformation trends derived from image correlation are consistent with field measurements, most field-measured coseismic displacements are systematically smaller than those obtained from image correlation. This discrepancy suggests that the 2025 Dingri earthquake likely produced a certain degree of off-fault deformation. Furthermore, the image correlation results indicate that the ratio of extensional to strike-slip displacement is approximately 2:1 for both average and maximum values. Based on this kinematic relationship, together with fault dip angles derived from inversion results reported in previous studies, the fault slip rake angle of the Dingri earthquake is estimated to range from -69° to -73°.

Key words: optical image correlation, Dingri earthquake, coseismic surface deformation, GF-2, Tibetan plateau

摘要：

准确量化同震断层滑动在近地表的分布特征, 对于认识地震破裂传播过程及断层结构演化至关重要。传统的野外实测和大地测量方法存在难以精确量化分散的区域性同震地表变形的问题。近年来, 光学卫星影像亚像素相关性匹配技术的迅速发展, 为高精度全面量化同震地表位移提供了新的解决方案。2025年1月7日, 西藏定日县发生 M_W7.1 强震, 造成了较大的人员伤亡和财产损失, 并沿丁木错断裂形成了长约35km的同震地表破裂带。为精确分析定日地震的同震地表变形特征, 文中利用震前和震后的中国高分二号(GF-2)光学卫星影像, 基于影像相关性匹配技术开展了同震位移定量研究。结果表明, 国产GF-2卫星影像在量化同震位移方面具有出色表现, 清晰地揭示了定日地震在尼辖错东北侧形成的长约6km的同震地表破裂带。影像匹配获得的同震地表变形场与野外调查结果共同揭示, 定日地震是一次伴随左行走滑分量的正断型地震事件, 尼辖错段地表破裂带EW向伸展量的平均值约为2m, 最大达3.9m, SN向左行走滑位移量的平均值约为0.9m, 最大达1.9m。根据伸展量与走滑量的比例关系, 结合断层倾角数据, 估算定日地震的断层滑动角约为-69°~-73°。

SU Qiang, PAN Jia-wei, LI Hai-bing, LIU Fu-cai, Marie-luce Chevalier, YANG Shao-hua, WU Kun-gang, JIANG Chen-yi. SURFACE DEFORMATION CHARACTERISTICS OF THE 2025 DINGRI M_W7.1 EARTHQUAKE DERIVED FROM GF-2 IMAGERY USING OPTICAL IMAGE CORRELATION TECHNIQUE[J]. SEISMOLOGY AND GEOLOGY, 2026, 48(4): 1035-1051.

苏强, 潘家伟, 李海兵, 刘富财, Marie-Luce Chevalier, 杨少华, 吴坤罡, 江晨轶. 基于GF-2影像相关性匹配的2025年 M_W7.1 西藏定日地震地表变形特征[J]. 地震地质, 2026, 48(4): 1035-1051.

Figures/Tables 10

Table1 Focal mechanisms of the Dingri earthquake from different institutions

北纬 /(°)	东经 /(°)	深度 /km	震级	节面Ⅰ/(°)			节面Ⅱ/(°)			资料来源
北纬 /(°)	东经 /(°)	深度 /km	震级	走向	倾角	滑动角	走向	倾角	滑动角	资料来源
28.50	87.45	10	M_S6.8(M_W7.1)	181	51	-81	348	40	-100	CENC ^①
28.639	87.361	10	M_W7.1	187	49	-78	349	42	-103	USGS ^②
28.56	87.47	12	M_W7.1	173	48	-92	356	42	-88	GCMT ^③
28.56	87.40	10	M_W7.1	164	41	-102	0	49	-79	GFZ ^④
28.53	87.40	10	M_W7.0	169	40	-94	355	50	-87	GA ^⑤
28.639	87.361	14	M_W7.2	196	44	-64	341	51	-113	IPGP ^⑥

Fig. 1 Geological and tectonic background map of the Dingri earthquake(after Kali, 2010; Leloup et al., 2010).

Table2 GF-2 optical image information used in this study

类别	采集时间	空间分辨率/m	含云量/%	侧摆角/(°)	偏航角/(°)	俯仰角/(°)
震前GF-2影像	2024-12-24,11:37	0.81	0	-0.006688	3.311295	0.000507
震后GF-2影像	2025-01-08,11:43	0.81	0	9.9193464	3.240400	0.000420

Fig. 2 Workflow for quantifying co-seismic displacement using optical image correlation technique.

Fig. 3 Co-seismic deformation field and surface rupture trace of the Dingri MW7.1 earthquake derived from correlation of GF-2 satellite images.

Fig. 4 Co-seismic displacement vector field of the Dingri earthquake, northeast of the Nixia Co.

Fig. 5 Field photographs showing typical surface deformation produced by the Dingri earthquake.

Fig. 6 Distribution of co-seismic displacement along the Nixia Co segment of the surface rupture zone produced by the Dingri earthquake.

Fig. 7 Comparison of co-seismic displacement derived from image correlation result to field measurements.

Fig. 8 Schematic diagram of fault slip.

References 57

[1]	卞爽, 于志泉, 龚俊峰, 等. 2021. 青藏高原近SN向裂谷的时空分布特征及动力学机制[J]. 地质力学学报, 27(2): 178-194.
	BIAN Shuang, YU Zhi-quan, GONG Jun-feng, et al. 2021. Spatiotemporal distribution and geodynamic mechanism of the nearly NS-trending rifts in the Tibetan plateau[J]. Journal of Geomechanics, 27(2): 178-194 (in Chinese).
[2]	邓起东. 2007. 中国活动构造图[CM]. 北京: 地震出版社.
	DENG Qi-dong. 2007. Active Tectonic Map of China[CM]. Seismological Press, Beijing (in Chinese).
[3]	黄婷, 吴中海, 韩帅, 等. 2024. 西藏日喀则地区的活断层基本特征及地震灾害潜在风险评估[J]. 地震科学进展, 54(10): 696-711.
	HUANG Ting, WU Zhong-hai, HAN Shuai, et al. 2024. The basic characteristics of active faults in the region of Xigaze, Xizang and the assessment of potential earthquake disaster risks[J]. Progress in Earthquake Sciences, 54(10): 696-711 (in Chinese).
[4]	李雨森, 李为乐, 许强, 等. 2025. 2025年1月7日西藏定日 M_S6.8 地震InSAR同震形变探测与断层滑动分布反演[J]. 成都理工大学学报(自然科学版), 52(2): 199-211.
	LI Yu-sen, LI Wei-le, XU Qiang, et al. 2025. InSAR co-seismic deformation detection and fault slip distribution inversion of the M_S6.8 earthquake in Dingri, Tibet on January 7, 2025[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 52(2): 199-211 (in Chinese).
[5]	刘富财, 潘家伟, 李海兵, 等. 2025. 2025年 M_W7.1 西藏定日地震地表破裂与同震位移分布特征[J]. 地质学报, 99(3): 685-703.
	LIU Fu-cai, PAN Jia-wei, LI Hai-bing, et al. 2025. Co-seismic surface rupture of the 2025 M_W7.1 Tingri earthquake and potential seismic risk in southern Tibetan plateau[J]. Acta Geologica Sinica, 99(3): 685-703 (in Chinese).
[6]	邵延秀, 王爱生, 刘静, 等. 2025. 2025年1月7日西藏定日地震地表破裂特征和野外同震位移测量初步结果[J]. 地球科学, 50(5): 1677-1695.
	SHAO Yan-xiu, WANG Ai-sheng, LIU Jing, et al. 2025. Preliminary investigation on surface rupture and coseismic displacement of the January 7, 2025, Dingri earthquake in Xizang[J]. Earth Science, 50(5): 1677-1695 (in Chinese).
[7]	石峰, 梁明剑, 罗全星, 等. 2025. 2025年1月7日西藏定日6.8级地震发震构造与同震地表破裂特征[J]. 地震地质, 47(1): 1-15. doi: 10.3969/j.issn.0253-4967.2025.01.001.
	SHI Feng, LIANG Ming-jian, LUO Quan-xing, et al. 2025. Seismogenic fault and coseismic surface deformation of the Dingri M_S6.8 earthquake in Tibet, China[J]. Seismology and Geology, 47(1): 1-15 (in Chinese). DOI
[8]	谭莎莎, 杨莹辉, 许强, 等. 2025. 2025年1月7日西藏定日县 M_S6.8 强震地表同震形变特征与房屋建筑震损分析[J]. 成都理工大学学报(自然科学版), 52(2): 212-222.
	TAN Sha-sha, YANG Ying-hui, XU Qiang, et al. 2025. Coseismic deformation and seismic damage assessment of buildings from the M_S6.8 earthquake in Dingri, Xizang, on January 7, 2025[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 52(2): 212-222 (in Chinese).
[9]	田婷婷. 2021. 申扎-定结裂谷南段丁木错断裂晚第四纪古地震事件研究[D]. 北京: 中国地质大学(北京).
	TIAN Ting-ting. 2021. Dating of late Quaternary paleoseismic events of the Dingmu Cuogao Fault in the southern section of Shenzha-Dingjie Rift[D]. China University of Geosciences(Beijing), Beijing (in Chinese).
[10]	田婷婷, 吴中海. 2023. 西藏申扎-定结裂谷南段丁木错正断层的最新史前大地震事件及其地震地质意义[J]. 地质论评, 69(S1): 53-55.
	TIAN Ting-ting, WU Zhong-hai. 2023. Recent prehistoric major earthquake event of Dingmucuo normal fault in the southern segment of Shenzha-Dingjie Rift and its seismic geological significance[J]. Geological Review, 69(S1): 53-55 (in Chinese).
[11]	王楠, 李永生, 申文豪, 等. 2025. 2025年1月7日西藏定日 M_S6.8 地震震源机制InSAR反演及强地面运动快速模拟[J]. 武汉大学学报(信息科学版), 50(2): 404-411.
	WANG Nan, LI Yong-sheng, SHEN Wen-hao, et al. 2025. Source parameters and rapid simulation of strong ground motion of the M_S6.8 earthquake on January 7, 2025, in Dingri(Xizang, China)derived from InSAR observation[J]. Geomatics and Information Science of Wuhan University, 50(2): 404-411 (in Chinese).
[12]	吴中海, 赵希涛, 吴珍汉, 等. 2005. 西藏安多-错那湖地堑的第四纪地质、断裂活动及其运动学特征分析[J]. 第四纪研究, 25(4): 490-502.
	WU Zhong-hai, ZHAO Xi-tao, WU Zhen-han, et al. 2005. Active faults and their kinematic features at the Amdo-Tsona Graben, central Xizang[J]. Quaternary Sciences, 25(4): 490-502 (in Chinese).
[13]	徐心悦. 2019. 藏南申扎-定结断裂系卡达正断裂晚第四纪活动性及其环境效应[D]. 北京: 中国地震局地质研究所.
	XU Xin-yue. 2019. Late Quaternary activity and its environmental effects of the N-S trending Kharta Fault in Xainza-Dinggye rift, Southern Tibet[D]. Institute of Geology, China Earthquake Administration, Beijing (in Chinese).
[14]	张进江, 丁林. 2003. 青藏高原EW向伸展及其地质意义[J]. 地质科学, 38(2): 179-189.
	ZHANG Jin-jiang, DING Lin. 2003. East-west extension in Tibetan plateau and its significance to tectonic evolution[J]. Chinese Journal of Geology, 38(2): 179-189 (in Chinese).
[15]	张进江, 郭磊, 丁林. 2002. 申扎-定结正断层体系中, 南段构造特征及其与藏南拆离系的关系[J]. 科学通报, 47(10): 738-743.
	ZHANG Jin-jiang, GUO Lei, DING Lin. 2002. Structural characteristics of the southern segment in the Shenzha-Dingjie normal fault system and its relationship with the southern Tibetan detachment system[J]. Chinese Science Bulletin, 47(10): 738-743 (in Chinese).
[16]	Armijo R, Tapponnier P, Mercier J, et al. 1986. Quaternary extension in southern Tibet: Field observations and tectonic implications[J]. Journal of Geophysical Research: Solid Earth, 91(B14): 13803-13872.
[17]	Avouac J-P, Ayoub F, Wei S, et al. 2014. The 2013, M_W7.7 Balochistan earthquake, energetic strike-slip reactivation of a thrust fault[J]. Earth and Planetary Science Letters, 391: 128-134. DOI URL
[18]	Ayoub F, Leprince S, Avouac J-P. 2009. Co-registration and correlation of aerial photographs for ground deformation measurements[J]. ISPRS Journal of Photogrammetry and Remote Sensing, 64(6): 551-560. DOI URL
[19]	Baird T, Bristow C S, Vermeesch P. 2019. Measuring sand dune migration rates with COSI-Corr and Landsat: Opportunities and challenges[J]. Remote Sensing, 11(20): 2423. DOI URL
[20]	Copley A, Faridi M, Ghorashi M, et al. 2014. The 2012 August 11 Ahar earthquakes: Consequences for tectonics and earthquake hazard in the Turkish-Iranian Plateau[J]. Geophysical Journal International, 196(1): 15-21. DOI URL
[21]	Cournet M, Giros A, Dumas L, et al. 2016. 2d sub-pixel disparity measurement using QPEC/Medicis[J]. The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 41: 291-298.
[22]	Debella-Gilo M, Kääb A. 2011. Sub-pixel precision image matching for measuring surface displacements on mass movements using normalized cross-correlation[J]. Remote Sensing of Environment, 115(1): 130-142. DOI URL
[23]	Dozier J, Frew J. 1990. Rapid calculation of terrain parameters for radiation modeling from digital elevation data[J]. IEEE Transactions on Geoscience and Remote Sensing, 28(5): 963-969. DOI URL
[24]	Gan W, Zhang P, Shen Z K, et al. 2007. Present-day crustal motion within the Tibetan plateau inferred from GPS measurements[J]. Journal of Geophysical Research: Solid Earth, 112(B8): B08416.
[25]	Gaudreau É, Hollingsworth J, Nissen E, et al. 2023. Complex 3-D surface deformation in the 1971 San Fernando, California earthquake reveals static and dynamic controls on off-fault deformation[J]. Journal of Geophysical Research: Solid Earth, 128(3): e2022JB024985.
[26]	Heid T, Kaab A. 2011. Evaluation of existing image matching methods for deriving glacier surface displacements globally from optical satellite imagery[J]. Remote Sensing of Environment, 118: 339-355. DOI URL
[27]	Hermas E, Leprince S, Abou El-Magd I. 2012. Retrieving sand dune movements using sub-pixel correlation of multi-temporal optical remote sensing imagery, northwest Sinai Peninsula, Egypt[J]. Remote Sensing of Environment, 121: 51-60. DOI URL
[28]	Hollingsworth J, Ye L, Avouac J P. 2017. Dynamically triggered slip on a splay fault in the M_W7.8, 2016 Kaikoura(New Zealand)earthquake[J]. Geophysical Research Letters, 44(8): 3517-3525. DOI URL
[29]	Huang M, Zhou Y, Lu L, et al. 2020. Some thoughts on measuring earthquake deformation using optical imagery[J]. IEEE Transactions on Geoscience and Remote Sensing, 58(2): 1052-1062. DOI
[30]	Jessup M J, Newell D L, Cottle J M, et al. 2008. Orogen-parallel extension and exhumation enhanced by denudation in the trans-Himalayan Arun River gorge, Ama Drime Massif, Tibet-Nepal[J]. Geology, 36(7): 587-590. DOI URL
[31]	Kali E. 2010. De la deformation long-terme a court-terme sur les failles normales du Sud-Tibet: Approche geochronologique multi-methodes (¹⁰Be, ²⁶Al, (U-Th)/He, ⁴⁰Ar/³⁹Ar, U/Pb)[D]. Universite de Strasbourg, Strasbourg.
[32]	Konca A O, Leprince S, Avouac J-P, et al. 2010. Rupture process of the 1999 M_W7.1 Duzce earthquake from joint analysis of SPOT, GPS, InSAR, strong-motion, and teleseismic data: A supershear rupture with variable rupture velocity[J]. Bulletin of the Seismological Society of America, 100(1): 267-288. DOI URL
[33]	Kuo Y T, Ayoub F, Leprince S, et al. 2014. Coseismic thrusting and folding in the 1999 M_W7.6 Chi-Chi earthquake: A high-resolution approach by aerial photos taken from Tsaotun, central Taiwan[J]. Journal of Geophysical Research: Solid Earth, 119(1): 645-660. DOI URL
[34]	Langille J M, Jessup M J, Cottle J M, et al. 2010. Kinematic evolution of the Ama Drime detachment: Insights into orogen-parallel extension and exhumation of the Ama Drime Massif, Tibet-Nepal[J]. Journal of Structural Geology, 32(7): 900-919. DOI
[35]	Leloup P H, Maheo G, Arnaud N, et al. 2010. The South Tibet detachment shear zone in the Dinggye area: Time constraints on extrusion models of the Himalayas[J]. Earth and Planetary Science Letters, 292(1-2): 1-16. DOI URL
[36]	Leprince S, Ayoub F, Klinger Y, et al. 2007a. Co-registration of optically sensed images and correlation(COSI-Corr): An operational methodology for ground deformation measurements[C]. 2007 IEEE International Geoscience and Remote Sensing Symposium, Barcelona, Spain: 1943-1946.
[37]	Leprince S, Barbot S, Ayoub F, et al. 2007b. Automatic and precise orthorectification, coregistration, and subpixel correlation of satellite images, application to ground deformation measurements[J]. IEEE Transactions on Geoscience and Remote Sensing, 45(6): 1529-1558. DOI URL
[38]	Massonnet D, Feigl K L. 1998. Radar interferometry and its application to changes in the Earth's surface[J]. Reviews of Geophysics, 36(4): 441-500. DOI URL
[39]	Michel R, Avouac J-P. 2002. Deformation due to the 17 August 1999 Izmit, Turkey, earthquake measured from SPOT images[J]. Journal of Geophysical Research: Solid Earth, 107(B4): ETG 2-1-ETG 2-6.
[40]	Milliner C W D, Dolan J F, Hollingsworth J, et al. 2015. Quantifying near-field and off-fault deformation patterns of the 1992 M_W7.3 Landers earthquake[J]. Geochemistry, Geophysics, Geosystems, 16(5): 1577-1598. DOI URL
[41]	Molnar P, Tapponnier P. 1975. 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]. Science, 189(4201): 419-426. PMID
[42]	Molnar P, Tapponnier P. 1978. Active tectonics of Tibet[J]. Journal of Geophysical Research: Solid Earth, 83(B11): 5361-5375.
[43]	Provost F, Michea D, Malet J-P, et al. 2022. Terrain deformation measurements from optical satellite imagery: The MPIC-OPT processing services for geohazards monitoring[J]. Remote Sensing of Environment, 274(4): 112949. DOI URL
[44]	Rockwell T K, Lindvall S, Dawson T, et al. 2002. Lateral offsets on surveyed cultural features resulting from the 1999 Izmit and Duzce earthquakes, Turkey[J]. Bulletin of the Seismological Society of America, 92(1): 79-94. DOI URL
[45]	Rosu A-M, Pierrot-Deseilligny M, Delorme A, et al. 2014. Measurement of ground displacement from optical satellite image correlation using the free open-source software MicMac[J]. ISPRS Journal of Photogrammetry and Remote Sensing, 10: 48-59.
[46]	Rupnik E, Daakir M, Pierrot-Deseilligny M. 2017. MicMac: A free, open-source solution for photogrammetry[J]. Open Geospatial Data, Software and Standards, 2(1): 14. DOI URL
[47]	Sandmeier S, Itten K I. 1997. A physically-based model to correct atmospheric and illumination effects in optical satellite data of rugged terrain[J]. IEEE Transactions on Geoscience and Remote Sensing, 35(3): 708-717. DOI URL
[48]	Scherler D, Leprince S, Strecker M R. 2008. Glacier-surface velocities in alpine terrain from optical satellite imagery: Accuracy improvement and quality assessment[J]. Remote Sensing of Environment, 112(10): 3806-3819. DOI URL
[49]	Stumpf A, Malet J-P, Delacourt C. 2017. Correlation of satellite image time-series for the detection and monitoring of slow-moving landslides[J]. Remote Sensing of Environment, 189: 40-55. DOI URL
[50]	Tapponnier P, Zhiqin X, Roger F, et al. 2001. Oblique stepwise rise and growth of the Tibet Plateau[J]. Science, 294(5547): 1671-1677. PMID
[51]	Travelletti J, Delacourt C, Allemand P, et al. 2012. Correlation of multi-temporal ground-based optical images for landslide monitoring: Application, potential and limitations[J]. ISPRS Journal of Photogrammetry and Remote Sensing, 70: 39-55. DOI URL
[52]	Van Puymbroeck N, Michel R, Binet R, et al. 2000. Measuring earthquakes from optical satellite images[J]. Applied Optics, 39(20): 3486-3494. PMID
[53]	Wang H, Elliott J R, Craig T J, et al. 2014. Normal faulting sequence in the Pumqu-Xainza Rift constrained by InSAR and teleseismic body-wave seismology[J]. Geochemistry, Geophysics, Geosystems, 15(7): 2947-2963. DOI URL
[54]	Yang W, Wang Y, Wang Y, et al. 2019. Retrospective deformation of the Baige landslide using optical remote sensing images[J]. Landslides, 17(3): 659-668. DOI
[55]	Yin A. 2000. Mode of Cenozoic east-west extension in Tibet suggesting a common origin of rifts in Asia during the Indo-Asian collision[J]. Journal of Geophysical Research: Solid Earth, 105(B9): 21745-21759.
[56]	Yin A, Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan orogen[J]. Annual Review of Earth and Planetary Sciences, 28(1): 211-280. DOI URL
[57]	Zitova B, Flusser J. 2003. Image registration methods: A survey[J]. Image and Vision Computing, 21(11): 977-1000. DOI URL