Please wait a minute...
 
REMOTE SENSING FOR LAND & RESOURCES    2004, Vol. 16 Issue (2) : 47-50,55     DOI: 10.6046/gtzyyg.2004.02.11
Technology Application |
REMOTE SENSING CHARACTERISTICS OF THE GEOMOPHIC DEFORMATION IN MID-NORTHERN QINGHAI-TIBET PALTEAU AND THEIR ECO-GEOLOGICAL SIGNIFICANCE
SUN Yan-gui1,2, YAO An-ping1, JU Sheng-cheng2, WANG-Dong-qing2, ZHANG-Kun2
1. Department of Geology, Northwest University, Xi'an 700069, China;
2. Center of Remote sensing, Qinghai Institute of Geological Survey, Xining 810012, China
Download: PDF(1380 KB)  
Export: BibTeX | EndNote | Reference Manager | ProCite | RefWorks    
Abstract  

Remote sensing geological features of Mid-northern Qinghai-Tibet plateau show that four NE-trending Quaternary depressions exist in the area between Lancangjiang-Wenquan and the southern margin of eastern Kunlun-Animaqing lithospheric faults. The graben geomorphic characteristics of Northern Xiqiangtang and Changjiang Riverhead depressions are obvious, whereas the Huanghe Riverhead and Ruoergai depressions are of relatively low development degree. However, they are products of the east-west geomorphic extensive deformation, and the dynamic background of the deformation is the same as that of the continental tectonic deformation of Qinghai-Tibet plateau. Studies further show that the deformation of these depressions not only has the same dynamic significance as the NS-trending rifts in mid-southern Qinghai-Tibet plateau but also serve as important factors affecting the ecological system of that region.

Issue Date: 02 August 2011
Service
E-mail this article
E-mail Alert
RSS
Articles by authors
Wang Pinqing
Cite this article:   
Wang Pinqing. REMOTE SENSING CHARACTERISTICS OF THE GEOMOPHIC DEFORMATION IN MID-NORTHERN QINGHAI-TIBET PALTEAU AND THEIR ECO-GEOLOGICAL SIGNIFICANCE[J]. REMOTE SENSING FOR LAND & RESOURCES, 2004, 16(2): 47-50,55.
URL:  
https://www.gtzyyg.com/EN/10.6046/gtzyyg.2004.02.11     OR     https://www.gtzyyg.com/EN/Y2004/V16/I2/47


[1] 张国伟,董云鹏,姚安平.关于中国大陆动力学与造山带研究的几点思考[J].中国地质,2002,29(1):7-13.




[2] 许志琴,杨经绥,姜枚,等.大陆俯冲作用及青藏高原周缘造山带的崛起[J].地学前缘,1999,6(3):139-152.




[3] 刘和莆,夏义平,殷进根,等.走滑造山带与盆地耦合机制[J]. 地学前缘,1999,6(3):121-132.




[4] 蔡学林,曹家敏,刘援朝,等.青藏高原多向碰撞-楔入隆升地球动力学模式[J]. 地学前缘,1999,6(3):181-189.




[5] An Yin, Paul Kaap A, Michael Murpny A, et al..Significant late Neogene east-west extension in northern Tibet[J].Geology,1999,27(9):787-790.




[6] Carmala N Garzione, David L.Dettman, Jay Quade, et al..High times on the Tibetan Plateau:Paleoelevation of the Thakkhola graben,Nepal[J]. Geology,2000,28(4):339-342.




[7] Helen Williams, Simon Turmer,Simon Kelley, et al..Age and composition of dikes in Southern Tibet:New constraints on the timing of east-west extension and its relationship to postcollisional volcanism[J]. Geology,2001,29(4):339-342.




[8] Blisniuk P M, Siwen S, Kuchel O,et al..Late Neogene extension in the Shuang Hu graben,central Tibet[J]. EOS,1998,79:794.




[9] Beghoul N, Barazangi B L.Lithospheric structure of Tibet and western north America:mechanisms of uplift and comparative study[J].Journal of Geophysical Research,1993,98:1997-2016.




[10] Mattauer M.Intracontinental subduction,crust mantle decollement and crustal stacking wedge in the Himalayan and other collision belts[J].Spec Publ J Geol Soc London,1986,19:37-50.




[11] Molnar P.A review of geophysical constraints on the deep structure of the Tibet Plateau,the Himalaya and the Karakoram,and their tectonic implications[J].Phil Trans R Soc Lond,1988,A326:33-38.




[12] Zhao W L, Morgan W J.Uplift of the Tibet Plateau[J].Tectonics,1985,4:359-369.




[13] 许志琴,姜枚,杨经绥.青藏高原北部隆升的深部构造物理作用[J].地质学报,1996,70(3):195-206.




[14] 潘裕生.青藏高原的形成与隆升[J]. 地学前缘,1999,6(3):153-162.




[15] 邓万明,孙宏娟.青藏高原的形成与隆升[J].地质论评,1999,45(增刊):952-958.




[16] 潘保田,李吉均.青藏高原:全球气候变化的驱动机与放大器[J].兰州大学学报(自然科学版),1996,32(1):108-115.




[17] 施雅风,李吉均,李炳元,等.晚新生代青藏高原的隆升与东亚环境变化[J].地理学报,1999,54(1):10-21.




[18] 张兰生,方修琦,任国玉.全球变化[M].北京:高等教育出版社,2000.




[19] An Zhisheng,John E Kutzbach,Warren L Prell,et al..Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times[J].Nature,2001,411:62-66.




[20] Dianfa Zhang, Fengquan L, Jianmin B.Eco-environmental effects of the Qinghai-Tibet Plateau uplift during the Quaternary in China.Environment[J]. Geology,2000,39(12):1352-1358.




[21] Houseman G A, McKenzie D P, Molnar P.Convective thinning of a thickened boundary layer and its relevance for the thermal evolution of continental convergent belts[J].Journal of Geophysical Research,1981,86:6115-6132.




[22] England P, Houseman G.Finite strain calculations of continental deformation 2.Comparison with the India-Asia collision zone[J]. Journal of Geophysical Research,1986,91:3664-3676.




[23] McCaffrey R, Nabelek J.Role of oblique convergence in the active deformation of the Himalayas and southern Tibet Plateau[J].Geology,1998,26:691-694.




[24] Yin A.Mode of Cenozoic east-west extension in Tibet suggesting a common origin of rift in Asia during the Indo-Asia collision[J].Journal of Geophysical Research,2000,105:21754-21759.




[25] Marin K C, Leigh H R.Topographic ooze:Building the eastern margin of Tibet by lower crustal flow[J].Geology,2000,28(8):703-706.




[26] Holt W E.Correlated crust and mantle strain field in Tibet[J].Geology,2000,28(1):67-70.




[27] Chen W P, Ozalaybey S.Correlation between seismic anisotropy and Bouguer gravity anomalies in Tibet and its implications for lithospheric structures[J]. Geophys.J.Int., 1998,135:97-101.




[28] Alstorf D, Brown L, Nelson K D,et al..Crustal deformation of the Lhasa terrane, Tibet plateau from project INDEPTH deep seismic reflection profiles[J].Tectonics, 1998,17:501-519.




[29] Xue G Q, Qian H, Jiang M, et al..Studies on the velocity structure of crust-upper mantle beneath the eastern Qinghai-Tibet plateau using seismic tomogeaphy[J].Continental Dynamics, 1999,4(2):79-85.




[30] 王琪,张培震,牛之俊,等.中国大陆现今地壳运动和构造变形[J].中国科学(D辑),2001,31(7):529-536.




[31] Karakhanian K, Tozalakyan P, Grillot J C, et al..Tectonic impact on the Lake Sevan environment (Armenia)[J].Environmental Geology,2001,40(3):279-288.




[32] 许志琴,李海兵,杨经绥,等.东昆仑山南缘大型转换挤压构造带和斜向俯冲作用[J].地质学报,2001,75(2):156-164.




[33] 许志琴,杨经绥,姜枚,等.青藏高原北部的碰撞造山及深部动力学[J].地球学报,2001,22(1):5-10.




[34] 张以弗,郑健康.青海可可西里及邻区地质概论[M].北京:地震出版社,1994.




[35] 刘树根.龙门山冲断带与川西前陆盆地的形成演化[M].成都:成都科技大学出版社,1993.




[36] Trofimov V T.Ecological Geology-A novel branch of geological sciences[J].地学前缘,2000,8(1):27-35.




[37] 孙延贵,张显廷,张琨,等.遥感技术在青藏高原北部生态环境调查中的应用[J].青海地质,2001,10(增刊):56-61.




[38] 曹明奎,李克让.陆地生态系统与气候相互作用的研究进展[J].地球科学进展,2000,15(4):446-451.

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
京ICP备05055290号-2
Copyright © 2017 Remote Sensing for Natural Resources
Support by Beijing Magtech