Please wait a minute...
img

Wechat

Remote Sensing Technology and Application  2012, Vol. 27 Issue (2): 265-274    DOI: 10.11873/j.issn.1004-0323.2012.2.265
    
The Study of Structural Interpretation based on Worldview-Ⅱ Remote Sensing Image in Gaize,Tibet and Its Application
Zhang Ruisi1,2,Chen Jianping1,2,Zeng Min3
(1.School of Earth Sciences and Resources,Beijing 100083,China;2.Key Laboratory of Research and Exploration Information of Land Resources,Beijing 100083,China;3.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China)
Download:  PDF (6926KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  

This paper introduces the image processing methods of Worldview-Ⅱ image data and the study on the interpreting of structure.By employing ETM+ and Worldview-Ⅱ remote sensing images,with geomorphic analysis,to carry out structural interpretation in Gaize area,west-central Tibet,China.It is the first time to do such big range of remote sensing interpreting on the Gaize area,where is at high altitude,and difficult to deploy the ground work in.The results suggested that the interpretation works have gotten the good results based on Worldview-Ⅱ remote sensing images.And according to the results,there are three types of fault structures developed in the area,i.e.E-striking thrusts,N-striking normal faults and NE- or NW-striking strike-slip faults,in response to the prevailing stress regime of N-S maximum stress and W-E minimum stress that results in the N-S contraction and W-E tension in Tibet.Remarkable geomorphic features have been controlled by the fault structures:① the Relacuo lake to the north of the Gaize town is developed on a graben bounded by N-S striking normal faults;② the Xiagacuo lake is formed on a bend-release basin as a result of the transtensional horsetail termination of a NW trending dextral strike-slip fault;③the fluvial plain to the north of Gaize is controlled by a NE-trending transtensional sinistral strike-slip fault.

Key words:  Bangong&mdash      Nujiang suture      Gaize      Remote sensing image      Structural interpretation      Worldview-Ⅱ     
Received:  21 December 2011      Published:  23 January 2013
P 542.3  
  TP 79  
Service
E-mail this article
Add to my bookshelf
Add to citation manager
E-mail Alert
RSS
Articles by authors

Cite this article: 

. The Study of Structural Interpretation based on Worldview-Ⅱ Remote Sensing Image in Gaize,Tibet and Its Application. Remote Sensing Technology and Application, 2012, 27(2): 265-274.

URL: 

http://www.rsta.ac.cn/EN/10.11873/j.issn.1004-0323.2012.2.265     OR     http://www.rsta.ac.cn/EN/Y2012/V27/I2/265

[1]Purkis S J,Riegl B M,Andrefouet S.Remote Sensing of Geomorphology and Facies Patterns on a Modern Carbonate Ramp (Arabian Gulf,Dubai,UAE)[J].Journal of Sedimentary Research,2005,75(5):861-876.
[2]Snidero M,Amilibia A,Gratacos O,et al.The 3D Reconstruction of Geological Structures based on Remote Sensing Data:Example from the Anaran Anticline,Lurestan Province,Zagros Fold and Thrust Belt,Lran[J].Journal of the Geological Society,2011,168(3):769-782.
[3]Rowan L C,Mars J C,Simpson C J.Lithologic Mapping of the Mordor,NT,Australia Ultramafic Complex by Using the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER)[J].Remote Sensing of Environment,2005,99(1-2):105-126.
[4]Burbank D W,Anderson R S.Tectonic Geomorphology[M].Berlin:Blackwell Science,2001:274.
[5]Sanchez V I,Murphy M A,Dupr E W R,et al.Structural Evolution of the Neogene Gar Basin,Western Tibet:Implications for Releasing Bend Development and Drainage Patterns[J].Geological Society of America Bulletin,2010,122(5-6):926-945.
[6]Taylor M,Yin A,Ryerson F J,et al.Conjugate Strike-slip Faulting along the Bangong—Nujiang Suture Zone Accommodates Coeval East-west Extension and North-south Shortening in the Interior of the Tibetan Plateau[J].Tectonics,2003,22(4):1044-1064.
[7]Kapp P,Yin A,Harrison T M,et al.Cretaceous-Tertiary Shortening,Basin Development and Volcanism in Central Tibet[J].Bulletin of the Geological Society of America,2005,117(7-8):865-878.
[8]Ji Peng,Guo Huadong,Zhang Lu.Landsat based Dynamic Area Change of the Glaciers to the North of the Guozhacuo Lake,1991~2009[J].Remote Sensing Technology and Application,2011,26(2):202-208.[纪鹏,郭华东,张露.基于Landsat数据的郭扎错北面冰川近20年来面积动态变化遥感研究[J].遥感技术与应用,2011,26(2):202-208.]
[9]Ren Jishun,Xiao Liwei.Lifting the Mysterious Veil of the Tectonics of the Qinghai—Tibet Plateau by 1∶250 000 Geological Mapping[J].Regional Geology of China,2004,23(1):1-11.[任纪舜,肖黎薇.1∶25 万地质填图进一步揭开了青藏高原大地构造的神秘面纱[J].地质通报,2004,23(1):1-11.]
[10]Yin A,Harrison T M.Geologic Evolution of the Himalayan-Tibetan Orogen[J].Annual Review of Earth and Planetary Sciences,2000,28(1):211-280.
[11]Wu Zhenhan,Ye Peisheng,Hu Daogong,et al.Paleogene Thrust System in Southern Qiangtang Basin,Central Tibetan Plateau[J].Regional Geology of China,2011,31(7):1009-1016.[吴珍汉,叶培盛,胡道功,等.青藏高原羌塘盆地南部古近纪逆冲推覆构造系统[J].地质通报,2011,31(7):1009-1016.]
[12]Zhang K J,Xia B,Liang X.Mesozoic——Paleogene Sedimentary Facies and Paleogeography of Tibet,Western China:Tectonic Implications[J].Geological Journal.2002,37(3):217-246.
[13]Zhang Yuxiu.Tectonic Evolution of the Middle-western Ban-gong-Nujiang Suture,Tibet[D].Beijing:Chinese Academy of Sciences,2007.[张玉修.班公湖——怒江缝合带中西段构造演化[D].北京:中国科学院研究生院,2007.]
[14]Dewey J F,Shackleton R M,Cheng F C,et al.The Tectonic Evolution of the Tibetan Plateau[J].Philosophical Transactions of the Royal Society of London.Series A,Mathematical and Physical Sciences,1988,327(1594):379-413.
[15]Schneider W,Mattern F,Wang P.Tectonic and Sedimentary Basin Evolution of the Eastern Bangong-Nujiang Zone (Tibet):A Reading Cycle[J].International Journal of Earth Sciences (Geologische Rundschau),2003,92:228-254.
[16]Shi D,Zhao W,Brown L,et al.Detection of Southward Intracontinental Subduction of Tibetan Lithosphere along the Bangong—Nujiang Suture by P-to-S Converted Waves[J].Geology,2004,32(3):209-212.
[17]Zhu D,Zhao Z,Niu Y,et al.The Lhasa Terrane:Record of a Microcontinent and Its Histories of Drift and Growth[J].Earth and Planetary Science Letters,2011,301(1-2):241-255.
[18]Zhu Dicheng,Pan Guitang,Mo Xuanxue,et al.Late Jurassic-Early Cretaceous Geodynamic Setting in Middle-northern Gangdese:New Insights from Volcanic Rocks[J].Acta Petrologica Sinica,2006,(3):534-546.[朱弟成,潘桂棠,莫宣学,等.冈底斯中北部晚侏罗世—早白垩世地球动力学环境:火山岩约束[J].岩石学报,2006,(3):534-546.]
[19]Pan Guitang,Ding Jun,Yao Dongsheng,et al.Instructions of the Qinghai-Tibet Plateau and Adjacent Areas Geological Chengdu Map[M].Chengdu:Chengdu Cartographic Publishing House,2004:1-47.[潘桂棠,丁俊,姚东生,等.青藏高原及邻区地质图说明书[M].成都:成都地图出版社,2004:1-47.]
[20]Zhang K J,Xia B D,Wang G M,et al.Early Cretaceous Stratigraphy,Depositional Environments,Sandstone Provenance,and Tectonic Setting of Central Tibet,Western China[J].Bulletin of the Geological Society of America,2004,116(9-10):1202-1222.
[21]Kapp P,Decelles P G,Gehrels G E,et al.Geological Records of the Lhasa—Qiangtang and Indo-Asian Collisions in the Nima Area of Central Tibet[J].Geological Society of America Bulletin,2007,119(7-8):917-932.
[22]Yin A.Cenozoic Tectonic Evolution of Asia:A Preliminary Synthesis[J].Tectonophysics,2010,488(1-4):293-325.
[23]Cao Jianjun.Study on Fusion of Aerial and TM Image and Its Application[J].Remote Sensing Technology and Application,2002,17(6):394-397.[曹建君.航空影像和TM 影像融合及应用研究[J].遥感技术与应用,2002,17(6):394-397.]
[24]Zhu Liangpu.Remote Sensing Geology[M].Beijing:Geological Publishing House,2009.[朱亮璞.遥感地质学[M].北京:地质出版社,2009.]
[25]〖KG*7/8〗Twiss R J,Morres E M.Structural Geology[M].United Kingdom:Cambridge University Press,2007:749.
[26]Kapp P,Yin A,Manning C E,et al.Tectonic Evolution of the Early Mesozoic Blueschist-bearing Qiangtang Metamorphic Belt,Central Tibet[J].Tectonics,2003,22(4):1043.
[27]Guynn J H,Kapp P,Pullen A,et al.Tibetan Basement Rocks Near Amdo Reveal“Missing” Mesozoic Tectonism along the Bangong Suture,Central Tibet[J].Geology,2006,34(6):505-508.

No Suggested Reading articles found!