Structural Analysis of the Hero Range in the Qaidam Basin, Northwestern China, Using Integrated UAV, Terrestrial LiDAR, Landsat 8, and 3-D Seismic Data

Quantitative structural analysis is a useful approach for studying geologic structures. It is particularly important in remote and complex fold-thrust belts where outcrop data and high-quality seismic reflection images are challenging to obtain. In this study, we integrated terrestrial light detection and ranging (LiDAR), unmanned aerial vehicle (UAV), and Landsat 8 (L8) data to extract high-resolution topographic and surface geologic information and constrain interpretations of three-dimensional (3-D) seismic reflection data in the Hero Range of the Qaidam Basin (QB) in northwestern China. UAV images were used to obtain a digital elevation model (DEM) and to measure the orientation of sedimentary bedding. Terrestrial LiDAR data were used to generate high-resolution digital outcrops and to evaluate the accuracy of the UAV-based DEM. L8 images were used to distinguish different stratigraphic units. The random sample consensus (RANSAC) algorithm was adopted to ascertain the best-fit plane of bedding. The results show that UAV images can be used to construct a DEM with <;1 m resolution and orthophotos with 0.15-m resolution. Collectively, these data improve the ability to identify and measure small exposures of bedding surfaces. The RANSAC algorithm improves the accuracy of measuring bedding orientations by removing erroneous selection points and facilitating the recognition of second-order variations in bedding orientation. The integrated analysis of remotely sensed and 3-D seismic data indicates that, of the three anticlines within the Hero Range, two are fault-propagation folds (the Shizigou and Youshashan anticlines) and one is associated with a pop-up structure (Ganchaigou anticline).

[1]  A. Yin,et al.  Cenozoic tectonic evolution of the Qaidam basin and its surrounding regions (Part 3): Structural geology, sedimentation, and regional tectonic reconstruction , 2008 .

[2]  Qiang Chen,et al.  Quantification of mass wasting volume associated with the giant landslide Daguangbao induced by the 2008 Wenchuan earthquake from persistent scatterer InSAR , 2014 .

[3]  Martha C. Anderson,et al.  Landsat-8: Science and Product Vision for Terrestrial Global Change Research , 2014 .

[4]  H. L. Vacher Computational Geology 12 – Cramer's Rule and the Three-Point Problem , 2000 .

[5]  K. Ruddick,et al.  Turbid wakes associated with offshore wind turbines observed with Landsat 8 , 2014 .

[6]  B. Burchfiel,et al.  Eastward migration of the Qaidam basin and its implications for Cenozoic evolution of the Altyn Tagh fault and associated river systems , 2006 .

[7]  S. Buckley,et al.  Terrestrial laser scanning in geology: data acquisition, processing and accuracy considerations , 2008, Journal of the Geological Society.

[8]  Shuhab D. Khan,et al.  Lidar mapping of faults in Houston, Texas, USA , 2008 .

[9]  Lin Ding,et al.  Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications , 2011 .

[10]  Xi-wei Xu,et al.  DEM and GIS analysis of geomorphic indices for evaluating recent uplift of the northeastern margin of the Tibetan Plateau, China , 2013 .

[11]  Kenneth J. W. McCaffrey,et al.  Quantitative analysis and visualization of nonplanar fault surfaces using terrestrial laser scanning (LIDAR)—The Arkitsa fault, central Greece, as a case study , 2009 .

[12]  Samuel T. Thiele,et al.  Ground-based and UAV-Based photogrammetry: A multi-scale, high-resolution mapping tool for structural geology and paleoseismology , 2014 .

[13]  A. C. Demirkesen Digital terrain analysis using Landsat‐7 ETM+ imagery and SRTM DEM: a case study of Nevsehir province (Cappadocia), Turkey , 2008 .

[14]  J. Pelletier,et al.  Wind erosion in the Qaidam basin, central Asia: Implications for tectonics, paleoclimate, and the source of the Loess Plateau , 2011 .

[15]  Graham Mills,et al.  Estimating the roughness of rock fractures and geomorphic surfaces by multiresolution analysis of terrestrial LiDAR data , 2013, Optical Metrology.

[16]  S. M. Jong,et al.  High-resolution monitoring of Himalayan glacier dynamics using unmanned aerial vehicles , 2014 .

[17]  D. Anderson,et al.  Geologic Stereo Mapping of Geologic Structures with SPOT Satellite Data: Geologic Note (1) , 1992 .

[18]  S. M. Jong,et al.  Mapping landslide displacements using Structure from Motion (SfM) and image correlation of multi-temporal UAV photography , 2014 .

[19]  J. M.R,et al.  UAV-based remote sensing of the Super-Sauze landslide : Evaluation and results , 2014 .

[20]  Z. Berger Geologic stereo mapping of geologic structures with SPOT satellite data , 1993 .

[21]  R. Baran,et al.  High-resolution spatial rupture pattern of a multiphase flower structure, Rex Hills, Nevada: New insights on scarp evolution in complex topography based on 3-D laser scanning , 2010 .

[22]  Kostas Stamatiou,et al.  Combining GeoEye-1 Satellite Remote Sensing, UAV Aerial Imaging, and Geophysical Surveys in Anomaly Detection Applied to Archaeology , 2011, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[23]  O. Fernández,et al.  Obtaining a best fitting plane through 3D georeferenced data , 2005 .

[24]  Daniel Reif,et al.  Quantitative structural analysis using remote sensing data: Kurdistan, northeast Iraq , 2011 .

[25]  Shuhab D. Khan,et al.  Application of multispectral LiDAR to automated virtual outcrop geology , 2014 .

[26]  K. Tansey,et al.  Lithological mapping of the Troodos ophiolite, Cyprus, using airborne LiDAR topographic data , 2010 .

[27]  L. Ding,et al.  Climatic and tectonic controls on sedimentation and erosion during the pliocene-quaternary in the qaidam basin (China) , 2013 .

[28]  Y. Dong,et al.  EW-trending uplifts along the southern side of the central segment of the Altyn Tagh Fault, NW China: Insight into the rising mechanism of the Altyn Mountain during the Cenozoic , 2012, Science China Earth Sciences.

[29]  E. Appel,et al.  Late Neogene magnetostratigraphy in the western Qaidam Basin (NE Tibetan Plateau) and its constraints on active tectonic uplift and progressive evolution of growth strata , 2013 .

[30]  M. Jaboyedoff,et al.  Spatio-temporal analysis of rockfall pre-failure deformation using Terrestrial LiDAR , 2014, Landslides.

[31]  O. Kreylos,et al.  Coseismic slip variation assessed from terrestrial lidar scans of the El Mayor–Cucapah surface rupture , 2013 .

[32]  Norbert Pfeifer,et al.  Landslide Displacement Monitoring Using 3D Range Flow on Airborne and Terrestrial LiDAR Data , 2013, Remote. Sens..

[33]  Ancheng Xiao,et al.  Impact of wind erosion on detecting active tectonics from geomorphic indexes in extremely arid areas: a case study from the Hero Range, Qaidam Basin, NW China , 2014 .

[34]  Danilo Schneider,et al.  Terrestrial lidar and hyperspectral data fusion products for geological outcrop analysis , 2013, Comput. Geosci..

[35]  S. Akciz,et al.  Applications of airborne and terrestrial laser scanning to paleoseismology , 2012 .

[36]  Jianxun Zhou,et al.  Cenozoic deformation history of the Qaidam Basin, NW China: Results from cross-section restoration and implications for Qinghai-Tibet Plateau tectonics , 2006 .

[37]  C. Kerans,et al.  Digital Outcrop Models: Applications of Terrestrial Scanning Lidar Technology in Stratigraphic Modeling , 2005 .

[38]  P. Kapp,et al.  Wind as the primary driver of erosion in the Qaidam Basin, China , 2013 .

[39]  Robert C. Bolles,et al.  Random sample consensus: a paradigm for model fitting with applications to image analysis and automated cartography , 1981, CACM.

[40]  David Green,et al.  Estimating Bedding Orientation From High-Resolution Digital Elevation Models , 2013, IEEE Transactions on Geoscience and Remote Sensing.

[41]  P. A. Brennan,et al.  Quantitative Structural Analysis with Stereoscopic Remote Sensing Imagery , 2000 .

[42]  An Yin,et al.  Geologic Evolution of the Himalayan-Tibetan Orogen , 2000 .

[43]  Y. Niu,et al.  Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling: The example of the North Qaidam UHPM belt, NW China , 2014 .

[44]  Piotr Zagórski,et al.  Use of terrestrial laser scanning (TLS) for monitoring and modelling of geomorphic processes and phenomena at a small and medium spatial scale in Polar environment (Scott River — Spitsbergen) , 2014 .

[45]  Damien Dhont,et al.  3-D modeling of geologic maps from surface data , 2005 .

[46]  Dimitri Lague,et al.  3D Terrestrial LiDAR data classification of complex natural scenes using a multi-scale dimensionality criterion: applications in geomorphology , 2011, ArXiv.

[47]  GIS as an aid to visualizing and mapping geology and rock properties in regions of subtle topography , 2005 .

[48]  S. Mitra,et al.  Remote surface mapping using orthophotos and geologic maps draped over digital elevation models: Application to the Sheep Mountain anticline, Wyoming , 2004 .

[49]  Nicola Casagli,et al.  Semi-automatic extraction of rock mass structural data from high resolution LIDAR point clouds , 2011 .

[50]  Kenji Omasa,et al.  Estimation and Error Analysis of Woody Canopy Leaf Area Density Profiles Using 3-D Airborne and Ground-Based Scanning Lidar Remote-Sensing Techniques , 2010, IEEE Transactions on Geoscience and Remote Sensing.

[51]  Ancheng Xiao,et al.  Late Jurassic–Early Cretaceous Northern Qaidam Basin, NW China: Implications for the earliest Cretaceous intracontinental tectonism , 2011 .