新生代构造变形,Cenozoic deformation
1)Cenozoic deformation新生代构造变形
英文短句/例句
1.Tectonic Deformation Characteristics and Structural Stress Simulation in Meso-Cenozoic Era in Northern Qaidam;柴北缘地区中新生代构造变形与构造应力场模拟
2.An Integrated Study on Late Cenozoic Tectonic Deformation in the Liupanshan-Madongshan Area, Northeastern Margin of the Tibetan Plateau青藏高原东北缘六盘山—马东山地区晚新生代构造变形综合研究
3.LATE CENOZOIC STRUCTURAL DEFORMATION FEATURES AND PETROLEUM OF WUSHI SAG OF TARIM BASIN,NW CHINA塔里木盆地乌什凹陷晚新生代构造变形特征与油气
4.Characteristics of the Cenozoic deformation in basin/range coupling regions on both sides of Tianshan Mountains and its geodynamics天山两侧山前新生代构造变形特征及其成因刍议
5.Analysis of Current Seismic Activity Features and Seismic Risk of Anhui Cenozoic Tectonic Deformation Zones Based on Seismic Activity Parameters由地震活动参数分析安徽省新生代构造变形带现今活动习性与地震危险性
6.CHARACTERISTICS OF CENOZOIC STRUCTURAL DEFORMATION IN NORTH MARGIN OF SOUTHWEST DEPRESSION, TARIM塔西南坳陷北缘新生代构造形变特征
7.DEFORMATION CHARACTERISTICS AND DISPLACEMENT AMOUNT OF THE LIANGSHAN ACTIVE FAULT ZONE IN LATE CENOZOIC ERA凉山活动构造带晚新生代变形特征与位移规模
8.Deformation History and Tectonic Evolution of Southeastern Tarim Basin in Mesozoic and Cenozoic塔里木盆地东南缘中新生代变形史与构造演化
9.Mesozoic deformation of Dabashan curvilinear structural belt of Qinling orogen秦岭造山带大巴山弧形构造带中生代构造变形
10.Structural Deformation and Tectonic Evolution of Harlik Mountain, in Xinjiang Since the Paleozoic;新疆哈尔里克山古生代以来构造变形及构造演化
11.Mesozoic-Cenozoic Superimposed Orogeny and Foreland Deformation in the Northeastern Sichuan Basin四川盆地东北部中—新生代造山与前陆变形构造叠合关系研究
12.In this paper, the deformation process and deformation mechanism of Qilianshan Structure Belt, since Cenozoic era, have been discussed.论述了祁连山构造带新生代以来的变形过程及形成机制。
13.Tectonic Deformation Features and Space-time Evolution in Northeastern Margin of the Qinghai-Tibetan Plateau Since the Late Cenozoic Time;青藏高原东北缘晚新生代以来的构造变形特征与时空演化
14.The Cenozoic tectonic evolution of the west Qinling:Constraints on the uplift and deformation of the Tibetan Plateau西秦岭新生代以来地质构造过程对青藏高原隆升和变形的约束
15.Structural style and deformation sequence of western Junggar, Xinjiang, since Late Paleozoic.新疆西准噶尔晚古生代以来构造样式与变形序列研究
16.Tectonic Model and Its Deformation Feature of Cenozoic in West Section of Lenghu Structural Belt, Northern Margin of Qaidam Basin冷湖构造带西段新生界构造模型及变形特征
17.A New Seismotectonic Belt:Features of the Latest Structural Deformation Style in the Mabian Seismotectonic Zone新生地震构造带——马边地震构造带最新构造变形样式的初步研究
18.Mesozoic Structure Deformation of the Chaobei Region,Anhui Province and Its Tectonic Setting安徽巢北地区的中生代构造变形及其大地构造背景
相关短句/例句
Cenozoic tectonic deformation zone新生代构造变形带
1.Based on the method of using a number of seismic activity parameters to determine activity features of fault zone segments,current seismic activity and seismic risk features of different segments ofCenozoic tectonic deformation zones in Anhui Province are analyzed.应用多个地震活动参数来判定断裂带分段落活动习性的方法,分析安徽省新生代构造变形带不同分段落的现今活动习性及地震危险性。
3)Cenozoic structures新生代构造
4)neotectonic deformation新构造变形
5)Late Cenozoic tectonic movement晚新生代构造
1.Late Cenozoic tectonic movement in the Keyir Mountain area,Kuqa,Xinjiang,and its controls on sandstone-type uranium deposits;新疆库车黑英山地区晚新生代构造运动及其对砂岩型铀矿成矿的控制作用初析
6)Cenozoic tectonic uplift新生代构造抬升
1.The globalCenozoic tectonic uplift, especially the uplift of Himalayan mountain beltTibet plateau in southern Asia,Andean mountain and Altiplano plateau in southern America, have the strong effects on the Earth surface chemical weathering and global climate change.全球新生代构造抬升 ,特别是南亚喜马拉雅青藏高原和南美安底斯山脉和Altiplano高原在新生代的抬升对地表化学风化和全球气候变化产生了重要影响。
延伸阅读
大坝内部变形观测(见水工建筑物变形观测)大坝内部变形观测(见水工建筑物变形观测)daba neibubianxing guanCe大坝内部变形观测见水工建筑物变形观测。
