About 67 item dissertation in line with tectonic deformation query results,the following is 1 to 50(Search took 0.046 seconds)

  1. The western edge of the Lanping basin lawn copper mining area tectonic deformation features and developmental mechanism,LiuQin/Kunming University of Science and Technology,0/42
  2. Study on Material Composition, Tectonic Evolution and Transformation at the Conjunction of Qinling and North Qilian Orogen,LiuChengJun/Chang'an University,0/22
  3. A Study on the Late Paleozoic Tectonic Framework and its Evolutionary Process in the Northern Margin of the West Qinling,WuShuKuan/Chang'an University,0/35
  4. The Material Composition,Structural Deformation and Geological Significance of Kobita Bea J Bai Bass Tao Paleozoic Accretionary Wedge,Qinghe County,Xinjiang,China,SunXiaoPan/Chang'an University,0/5
  5. Features of Structure Deformation and Evolution in the North Siziwangqi, Inner Mongolia,LiuZhiHui/Chinese Geology University (Beijing),0/2
  6. Composition, Structural Characteristics and Geological Evolution of North Qilian Orogen (the Eastern) in Early Paleozoic,WeiFangHui/Chang'an University,0/20
  7. Geological Characteristics and Tectonic Attribute of the Middle Proterozoic Metamorphic Rock Series in the Northern Margin of the Qaidam Basin,ZhengJun/Chang'an University,0/6
  8. Deep Electric Structure Beneath the Yingjiang-longling Area in Southwestern Yunnan and its Implications for Kinetics,YeTao/Institute of Geology of China Earthquake Administration,0/19
  9. Active tectonics and earthquake in northeastern Pamir Plateau Taxkorgan Valley,LiWenQiao/Institute of Geology of China Earthquake Administration,0/13
  10. Study on Present-day Crustal Movement with GPS Data and Modeling the Active Deformation in the Chinese Mainland,WangWei/China Seismological Bureau, Institute of Geophysics,0/266
  11. Surface Geomorphological Processes in the Northern Piedmont of Tian Shan Responding to Climate Change and Tectonic Deformation Since Middle Pleistocene,ChenZhengWei/Institute of Geology of China Earthquake Administration,0/38
  12. The Tectonic Deformation Characteristics and Ore-controlling Model of Yuele Lead-Zinc Deposit in Northeast Yunnan,HuangJianZi/Kunming University of Science and Technology,0/70
  13. Coalfield Structural and Tectonic Coal Controlling of North China Coal Hosting Area,LinZhongYue/Beijing,1/394
  14. Tectonics Analysis of BaiYinXiLe, Inner Mongolia Autonomous Region,ZuoZuoSen/Chinese Geology University (Beijing),0/35
  15. Research of Deep and Shallow Structural Features in the Upper Yangtze Region,ZhangYan/Northwestern University,0/68
  16. Geometric Pattern and Active Tectonics of the Hexi Corridor and Its Adjacent Regions,ZhengWenJun/Institute of Geology of China Earthquake Administration,0/91
  17. Jinchuan Mining Ductile Shear Zone Characteristics and Its Significance,MaJiaHong/Chang'an University,0/28
  18. A Study of Active Faults in Zhangjiakou Basin,ZhouJiangLin/China Seismological Bureau, Institute of Geophysics,0/88
  19. Study on Mechanisms and Characteristics of Major Faults in the Eastern Boundary of the Sichuan-Yunnan Block,WeiWenXin/Institute of Geology of China Earthquake Administration,0/123
  20. Active Thrusting and Folding along the Pamir Frontal Thrust System,LiTao/Institute of Geology of China Earthquake Administration,1/89
  21. Research on the Late Paleozoic-Early Mesozoic Orogeny in East Kunlun Orogen,LiRuiBao/Chang'an University,2/189
  22. The Early Paleozoic Tectonic Evolution of Kaladawan Area,Northern Altyn Taugh,LiSongBin/Chinese Academy of Geological Sciences,0/17
  23. Composition and Analysis of the Tectonic Deformation of Mélange Belt in Zhongba Area,Tibet,WangJinZhu/Chinese Geology University (Beijing),0/40
  24. Study on the Cause and Deformation Features of Quartz Veins in the Late Paleozoic Tectonic Schist,in Gangmari Region,Tibet,YaoYao/Chinese Geology University (Beijing),1/64
  25. Analysis of GPS Data with High Precision & Study on Present-day Crustal Deformation in China,WangMin/Institute of Geology of China Earthquake Administration,0/117
  26. Study of the Relationship between Tectonism and Petrogenesis and Metallization in Hetai Gold Mine Region, Western Guangdong,YueShi/Chinese Academy of Geological Sciences,0/136
  27. Yanshanian Tectonic Evolution of the Chengde Basin and the Adjacent Area in the Eastern Segment of the Yanshan Fold-and-thrust Belt,LiuJian/Chinese Academy of Geological Sciences,1/239
  28. Tectonic Deformation Characteristics and Structural Stress Simulation in Meso-Cenozoic Era in Northern Qaidam,ZhangXiJuan/Chinese Academy of Geological Sciences,1/493
  29. Numerical Simulations of Structural Deformations under Compressive Stress,ZhouYe/Guangzhou Institute of Geochemistry,1/423
  30. Discontinuous Motion and Deformation Models of Tectonic Block Systems and the Current Crustal Movement and Tectonic Stress Field in the Southern Tianshan Mountains Region,QinXiaoJun/Institute of Geology of China Earthquake Administration,0/274
  31. An Integrated Study on Late Cenozoic Tectonic Deformation in the Liupanshan-Madongshan Area, Northeastern Margin of the Tibetan Plateau,ZhangGuangLiang/Institute of Geology of China Earthquake Administration,1/479
  32. Cenozoic Tectonic Deformation and Evolution of the Northeastern Margin of the Tibetan Plateau: A Case Study of Longxi-Wushan Region,WangZhiCai/Institute of Geology of China Earthquake Administration,4/417
  33. A Study on the Characteristics of Recent Tectonic Deformation and Earthquake Activity in North China,TangFangTou/Institute of Geology of China Earthquake Administration,5/751
  34. Tectonic Deformation Features and Space-time Evolution in Northeastern Margin of the Qinghai-Tibetan Plateau Since the Late Cenozoic Time,YuanDaoYang/Institute of Geology of China Earthquake Administration,23/905
  35. Deep Electric Structures Beneath the Northeastern Margin of the Tibetan Plateau and Its Tectonic Implications,ZhanYan/Institute of Geology of China Earthquake Administration,3/253
  36. Kinematics of the Zhongwei Fault Zone in Middle-Late Quaternary,ChuQuanZhi/Institute of Geology of China Earthquake Administration,0/154
  37. Study on the Tectonic Deformation Characteristics and Geo-dynamics of Changle-nan’ao Metamorphic Zone,ShiJianJi/Chinese Geology University (Beijing),1/100
  38. The Research on Temporal and Spatial Distributions of Erosion Rates and Tectonic Deformation in the Northern Qilian Shan,HuXiaoFei/Lanzhou University,1/151
  39. Sedimentary Responses to the Cenozoic Tectonic Evolution of the Northeastern Corner of the Tibetan Plateau,WangWeiTao/Institute of Geology of China Earthquake Administration,0/116
  40. Tectonics Activity of the Nujiang Fault Zone in Quaternary in the Southwest Yunnan,LiGuangTao/China Seismological Bureau, Institute of Earthquake Prediction,0/164
  41. Studies on Tectonic Deformation of the Yellow River Terrace in Lanzhou Based on High-resolution GPS Surveying,LiuXingWang/Lanzhou Institute of Seismology , China Seismological Bureau,1/237
  42. Tibetan crustal deformation displacement back analysis model and Dynamic Simulation,ChenJianBing/Xi'an University of Science and Technology,0/224
  43. The Thrust Deformation of Pluton,WuJianYong/Zhejiang University,0/58
  44. Yanshan Epoch Tectonic Superposition in Changping Xuejiashiliang Region,ChenYiHan/Chinese Geology University (Beijing),1/91
  45. Analysis on Structural Characteristics in the Micangshan Area, NW Sichuan Basin,Guo/Zhejiang University,1/121
  46. Cenozoic Structure Features of Wupoer Area in Northeastern Margin of Pamir,ZhangFenFen/Zhejiang University,1/70
  47. A Study on Active Tectonics in the Yuexi Basin,ChenChangYun/Institute of Geology of China Earthquake Administration,0/61
  48. An Experimental Study of Crustal Rock Anisotropy,ZuoXiaoBing/Institute of Geology of China Earthquake Administration,1/117
  49. The Regional Tectonic Characteristic and Their Evolution of Metamorphic Rock Formation Kekesha Area in Dulan County, Qinghai,LiYanFeng/Chang'an University,1/88
  50. Structrural Character Research in the Northern Sichuan Basin,RanYongLiang/Chengdu University of Technology,1/290

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