PDF Download HTML

[1]CAI Xiaochao,TANG Hongtao.Precise Extraction of Quantitative Parameters of the Geological Structure in Pishan County,Xinjiang Using Oblique Photogrammetry[J].Journal of Seismological Research,2022,45(03):468-478.[doi:10.20015/j.cnki.ISSN1000-0666.2022.0047 ]

Copy

Precise Extraction of Quantitative Parameters of the Geological Structure in Pishan County,Xinjiang Using Oblique Photogrammetry

Journal of Seismological Research[ISSN 1000-0666/CN 53-1062/P] Volume: 45 Number of periods: 2022 03 Page number: 468-478 Column: 生命线工程系统抗震防灾专栏 Public date: 2022-06-20

Title:: Precise Extraction of Quantitative Parameters of the Geological Structure in Pishan County,Xinjiang Using Oblique Photogrammetry

Author(s):: CAI Xiaochao¹; TANG Hongtao²; (1.Henan Vocational College of Water Conservancy and Environment,Zhengzhou 450002,Henan,China)(2.The Second Monitoring and Application Center,China Earthquake Administration,Xi'an 710054,Shaanxi,China)

Keywords:: oblique photogrammetry; active structures; geomorphic interpretation; accuracy evaluation; quantitative parameters

CLC:: P642.22

DOI:: 10.20015/j.cnki.ISSN1000-0666.2022.0047

Abstract:: In this paper,the oblique photogrammetry technology is introduced into the quantitative research of geological active structures.Firstly,the basic principle of the data acquisition and processing of tilt photogrammetry is introduced,and the data acquisition and processing of the low-altitude,tilt photogrammetry are carried out in the study area of 20.08 km² in Pishan County,an earthquake-prone area in Xinjiang.The 3.39 cm high-resolution data of DOM,DSM,the 3D real scene modeling of 9 cm resolution,and DSM data such as contours,slopes are obtained.Secondly,according to 152 surface image control points,the accuracy of DOM and DSM data is evaluated,and the mean square error of the point plane is 1.7 cm,and the mean square error of elevation is 5.3 cm.Finally,with the help of the above-mentioned high-resolution digital model,the geomorphological interpretation of fault scarps in the study area was realized,and the vertical displacement of 7 terraces scarps was accurately extracted:F_1-2(3.71±0.62)m,F_2-3(3.54±0.04)m,F_3-4(6.06±0.22)m,F_4-5(7.43±0.56)m,F_5-6(5.52±0.18)m,F_6-7(13.05±0.33)m.Through oblique photogrammetry,the 3D real model,which is difficult to obtain by traditional aerial and satellite images,is directly obtained,and can be browsed and measured from any angle of view.The vertical displacement of terrace with real geographic coordinates is extracted too.The tilt photogrammetry technique has a broad application prospect in the quantitative study of geological active structures.

References:: 艾明,毕海芸,郑文俊,等.2018.利用无人机摄影测量技术提取活动构造定量参数[J].地震地质,40(6):1276-1293.
邓起东,陈立春,冉勇康.2004.活动构造定量研究与应用[J].地学前缘,11(4):383-392.
段宗恩,张海生.2019.单镜头倾斜摄影技术低成本三维建模[J].城市勘测,(4):129-131.
付碧宏,张松林,谢小平,等.2006.阿尔金断裂系西段:康西瓦断裂的晚第四纪构造地貌特征研究[J].第四纪研究,26(2):228-235.
李向东,王克卓.2002.西昆仑山北缘盆地构造转换解析[J].新疆地质,20(S1):19-25.
刘静,陈涛,张培震,等.2013.机载激光雷达扫描揭示海原断裂带微地貌的精细结构[J].科学通报,58(1):41-45.
潘家伟,李海宾,Van der Woerd J,等.2007.西昆仑山前冲断带晚新生代构造地貌特征[J].地质通报,26(10):1368-1379.
姚方芳.2014.基于倾斜影像的三维建模方法研究[D].泰安:山东科技大学.
俞晶星.2013.雅布赖山前断裂晚第四纪滑动速率与谷地震[D].北京:中国地震局地质研究所.
张玮,漆家福,雷刚林,等.2010.塔西南坳陷西昆仑山前冲断带的收缩构造变形模式[J].新疆石油地质,31(6):567-571.
张祖勋,吴军,张剑清.2003.建筑物场景三维重建中影像方位元素的获取方法[J].武汉大学学报(信息科学版),28(3):265-271.
Chen T,Zhang P Z,Liu J, et al.2014.Quantitative study of tectonic geomorphology along Haiyuan Fault based on airborne LiDAR[J].Chinese Science Bulletin,59(20):2396-2409.
Cunningham D,Grebby S,Tansey K, et al.2006.Application of airborne LiDAR to mapping seismogenic faults in forested mountainous terrain,southeastern Alps,Slovenia[J].Geophysical Research Letters,33(20):L20308.
Hamburger M W,Sarewitz D R,Pavlis T L, et al.1992.Structural seismic evidence for intracontinental subduction in the peter the First Range,Central Asia[J].Geological Society of America Bulletin,104(4):397-408.
Negredo A M,Replumaz A,Villasenor A, et al.2007.Modeling the evolution of continental subduction processes in the Pamir-Hindu Kush region[J].Earth and Planetary Science Letters,259(1-2):212-225.
Oskin M E,Arrowsmith J R,Corona A H, et al.2012.Near-field deformation from the EI Mayor-Cucapah earthquake revealed by differential LIDAR[J].Science,335(6069):702-705.
Peltzer G,Tapponnier P,Armijo R.1989.Magnitude of late Quaternary left-lateral displacements along the north edge of Tibet[J].Science,246(4935):1285-1289.
Qu G S,Li Y G,Li Y F, et al.2005.Segmentations of foreland belts and their tectonic mechanism in the southwest Tarim Basin[J].Science in China(Ser D),48(10):1585-1598.
Ren Z K,Zhang Z W,Chen T, et al.2016.Clustering of offsets on the Haiyuan Fault and their relationship to paleoearthquakes[J].Geological Society of America Bulletin,128(1-2):3-18.
Tapponnier P,Molnar P.1977.Active faulting and tectonics in China[J].Journal of Geophysical Research,82(20):2905-2930.
Tseng T L,Chen W P,Nowack R L.2009.Northward thinning of Tibetan crust revealed by virtual seismic profiles[J].Geophysical Research Letters,36(24):L24304doi:10.1029/2009GL040457.
Zielke O,Arrowsmith J R,Ludwig L G, et al.2010.Slip in the 1857 and earlier large earthquakes along the Carrizo Plain,San Andreas Fault[J].Science,327(5969):1119-1122.[LM]

Similar References:

Memo

Last Update: 2022-07-01