Morphotectonic Analyses of LiDAR-Derived DEMs: Insights into Tectonic Activity of the Xinhua Fault within the Three Gorges Area (Central China)

References

[1] BiH Y, ZhengW J, RenZ K, et al.. Using an Unmanned Aerial Vehicle for Topography Mapping of the Fault Zone Based on Structure from Motion Photogrammetry. International Journal of Remote Sensing, 2017, 38(8/9/10): 2495-2510

[2] BoultonS J, StokesM. Which DEM is Best for Analyzing Fluvial Landscape Development in Mountainous Terrains?. Geomorphology, 2018, 310: 168-187

[3] Chen, F., Wang, D., Yao, D. D., et al., 2024. Three Gorges Seismological Network: Monitoring Seismicity at the Three Gorges Reservoir Forebay. Seismological Research Letters, https://doi.org/10.1785/0220240228

[4] ChenJ H, YaoY S, WuH B, et al.. Research on ML 3.8 Small Earthquake Swarm in Three Gorges Reservoir Area on October 31, 2012. Journal of Geodesy and Geodynamics, 2013, 33(2): 31-34

[5] ChenT, LiuZ J, ShaoY X, et al.. Geomorphic Offsets along the Creeping Laohu Shan Section of the Haiyuan Fault, Northern Tibetan Plateau. Geosphere, 2018, 14(3): GES01561.1

[6] ChengY L, HeC Q, RaoG, et al.. Geomorphological and Structural Characterization of the Southern Weihe Graben, Central China: Implications for Fault Segmentation. Tectonophysics, 2018, 722: 11-24

[7] ChevalierM, LeloupP, ReplumazA, et al.. Temporally Constant Slip Rate along the Ganzi Fault, NW Xianshuihe Fault System, Eastern Tibet. GSA Bulletin, 2017, 130(3/4): 396-410

[8] DelcaillauB, GraveleauF, Saint CarlierD, et al.. Geomorphic Analysis of Active Fold Growth and Landscape Evolution in the Central Qiulitage Fold Belt, Southern Tian Shan, China. Geomorphology, 2022, 398: 108063

[9] DongS P, ZhangP Z, ZhangH P, et al.. Drainage Responses to the Activity of the Langshan Range-Front Fault and Tectonic Implications. Journal of Earth Science, 2018, 29(1): 193-209

[10] El HamdouniR, IrigarayC, FernándezT, et al.. Assessment of Relative Active Tectonics, Southwest Border of the Sierra Nevada (Southern Spain). Geomorphology, 2008, 96(1/2): 150-173

[11] GaoL, HeC Q, RaoG, et al.. Numerical Examination of the Geomorphic Indicators for Lateral Fold Growth. Geomorphology, 2023, 432: 108702

[12] HeC Q, RaoG, YangR, et al.. Divide Migration in Response to Asymmetric Uplift: Insights from the Wula Shan Horst, North China. Geomorphology, 2019, 339: 44-57

[13] HeC Q, YangC J, RaoG, et al.. Landscape Response to Normal Fault Linkage: Insights from Numerical Modeling. Geomorphology, 2021, 388: 107796

[14] HeC Q, YangC J, TurowskiJ M, et al.. Constraining Tectonic Uplift and Advection from the Main Drainage Divide of a Mountain Belt. Nature Communications, 2021, 12(1): 544

[15] HuX F, PanB T, KirbyE, et al.. Spatial Differences in Rock Uplift Rates Inferred from Channel Steepness Indices along the Northern Flank of the Qilian Mountain, Northeast Tibetan Plateau. Chinese Science Bulletin, 2010, 55(27): 3205-3214

[16] LiJ G, ZhangL F, LiaoW L, et al.. Earthquakes in the Fold Structure——the Genesis of the M4.3 Earthquake Sequence in the Three Gorges Reservoir Area in 2017. Chinese Journal of Geophysics, 2018, 61(9): 3701-3712(in Chinese with English Abstract)

[17] LiS L, YanZ G, XuJ R, et al.. First Microquake Swarm Activity since Storage in Three Gorges Reservoir. Journal of Geodesy and Geodynamics, 2003, 23(4): 75-79(in Chinese with English Abstract)

[18] LinZ, KanedaH, MukoyamaS, et al.. Detection of Subtle Tectonic–Geomorphic Features in Densely Forested Mountains by very High-Resolution Airborne LiDAR Survey. Geomorphology, 2013, 182: 104-115

[19] LiuJ, ChenT, ZhangP Z, et al.. Illuminating the Active Haiyuan Fault, China, by Airborne Light Detection and Ranging. Chinse Science Bulletin, 2013, 58(1): 41-45(in Chinese with English Abstract)

[20] OskinM E, ArrowsmithJ R, Hinojosa CoronaA, et al.. Near-Field Deformation from the El Mayor-Cucapah Earthquake Revealed by Differential LIDAR. Science, 2012, 335(6069): 702-705

[21] PanJ W, LiH B, ChevalierM L, et al.. Co-Seismic Rupture of the 2021, MW7.4 Maduo Earthquake (Northern Tibet): Short-Cutting of the Kunlun Fault Big Bend. Earth and Planetary Science Letters, 2022, 594: 117703

[22] Pérez-PeñaJ V, AzorA, AzañónJ M, et al.. Active Tectonics in the Sierra Nevada (Betic Cordillera, SE Spain): Insights from Geomorphic Indexes and Drainage Pattern Analysis. Geomorphology, 2010, 119(1/2): 74-87

[23] RaoG, HeC Q, ChenH L, et al.. Use of Small Unmanned Aerial Vehicle (sUAV) -Acquired Topography for Identifying and Characterizing Active Normal Faults along the Seerteng Shan, North China. Geomorphology, 2020, 359: 107168

[24] RaoG, HeC Q, ChenP, et al.. Active Normal Faulting along the Seerteng Shan, North China: Geometry and Kinematics. Journal of Asian Earth Sciences, 2019, 184: 103976

[25] RaoG, HeC Q, ChengY L, et al.. Active Normal Faulting along the Langshan Piedmont Fault, North China: Implications for Slip Partitioning in the Western Hetao Graben. The Journal of Geology, 2018, 126(1): 99-118

[26] RenZ K, ZhangZ Q, ChenT, et al.. Clustering of Offsets on the Haiyuan Fault and Their Relationship to Paleoearthquakes. Geological Society of America Bulletin, 2015, 128(1–2): 3-18

[27] SchwanghartW, ScherlerD. Short Communication: TopoToolbox 2 - MATLAB-Based Software for Topographic Analysis and Modeling in Earth Surface Sciences. Earth Surface Dynamics, 2014, 2(1): 1-7

[28] ShaoY X, ZhangB, ZouX B, et al.. Application of UAVLS to Rapid Geological Survey. Seismology and Geology, 2017, 39(6): 1185-1097(in Chinese with English Abstract)

[29] WangD, DongY P, XiZ P, et al.. Evaluation of the Relative Tectonic Activity from the Faults in the Gengma-Lancang-Menghai Seismic Belt (SouthWestern China). Journal of Earth Science, 2024, 35(1): 131-143

[30] WangD, YaoY S, XueJ R, et al.. Focal Mechanism of Key Monitoring Area of Three Gorges Reservoir before and after Impoundment. Journal of Geodesy and Geodynamics, 2007, 27(5): 103-107(in Chinese with English Abstract)

[31] WangQ L, ZhangL F, LiaoW L, et al.. Fault Tectonics and Seismic Activity Characteristics of Three Gorges Reservoir. Journal of Geodesy and Geodynamics, 2013, 33(5): 29-33(in Chinese with English Abstract)

[32] WangQ L, ZhangL F, LiaoW L, et al.. Research on Genesis of M4.2 and M4.5 Earthquake Sequences in March 2014 in Zigui County, Hubei Province. Seismology and Geology, 2016, 38(1): 121-130(in Chinese with English Abstract)

[33] WangY Z, ZhengD W, ZhangH P. The Methods and Program Implementation for River Longitudinal Profile Analysis—RiverProAnalysis, a Set of Open-Source Functions Based on the Matlab Platform. Science China Earth Sciences, 2022, 65(9): 1788-1809

[34] WestobyM J, BrasingtonJ, GlasserN F, et al.. ‘Structure-from-Motion’ Photogrammetry: A Low-Cost, Effective Tool for Geoscience Applications. Geomorphology, 2012, 179: 300-314

[35] WuY L, PeiJ L, WangZ, et al.. Analysis on the Characteristics of Crustal Structure and Seismotectonic Environment in Zigui Basin, Three Gorges. Frontiers in Earth Science, 2021, 9: 1085

[36] XiaJ W, ZhouL Q, ZhouJ Y. Relationship among Three Faults (Including the Shuibatian Fault) in Zigui, and Assessment of Seismogenic Intensities. Yangtze River, 1996, 27(1): 22-25(in Chinese with English Abstract)

[37] XiaJ W, ZhouL Q, LiuS Q. Study on the Fault Characteristics and Tectonic Activity in the Zigui Basin and Its Adjacent Regions, Western Hubei. Hydrogeology and Engineering Geology, 1996, 1: 10-14(in Chinese with English Abstract)

[38] ZielkeO, ArrowsmithJ R, LudwigL G, et al.. Slip in the 1857 and Earlier Large Earthquakes along the Carrizo Plain, San Andreas Fault. Science, 2010, 327: 1119-1122

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