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Based on the analysis of the geological tectonics setting and deep seated geophysical characteristics, the causative structure of the Yongdeng M S 5.8 earthquake on July 22, 1995 has been determined by the synthetical study of the faults in the earthquake area, focal mechanism solution, focal depths, meizoseismal region direction, post earthquake distribution, earthquake fissures and ground motion direction.

在分析地质构造背景和深部地球物理特征的基础上,通过对震区断裂构造、震源机制解、震源深度、极震区展布方向、余震空间分布、地震裂缝和地面运动方向的综合研究,确定了1995年7月22日永登5.8级地震的发震构造,探讨了形成该次地震的构造力学机制问题,认为该次地震是在局部构造应力直接作用下导致窑街—周家台隐伏断裂重新活动的结果

Among above deformation, the thrust-fold structure formed in Triassic established the E-W trend framework controlling the distribution of the late compressive settling. The NNE-NE trend obduction zone and regional folds is contributed to effect of Tethys tectonic region superimposed by Paleo-Pacific tectonic region.

其中三叠纪挤压变形产生的冲断—褶皱构造,奠定了本区中生代近东西向构造格局,并控制后期挤压坳陷型盆地的的空间展布规律;晚侏罗世早期挤压形成的北北东—北东向逆冲推覆构造带和区域性褶皱是特提斯构造域与古太平洋构造域共同叠加的结果。

Hechi-Yishan fault zone is located in the north of Guizhong depression, which general strike is NW-EW and consists of a series of obduction fault. Generally, there are two main faults, the fault-fold belt about 5-20km is made of main faults, subsidiary faults and concomitant folds; The dip of main faults is N or S; It can be divided into four different structural sections along its strike (Hechi section, Yishan section, Liucheng section and Yingshan section). There are some differences among these sections in structure characteristic, such as fault structure, associated structure, fold association style, deformation of rock, and so on.

河池-宜山断裂带展布于桂中坳陷北部,总体走向NW-近EW 向,由一系列逆冲断层组成,主干断裂一般为2条,主干断裂与次级断裂及伴随的褶皱构造构成宽5-20km 不等的断褶带;主断裂倾向N 或S;沿走向可分为河池、宜山、柳城、英山四个构造段;各段断裂结构、伴生构造、褶皱组合样式、岩石变形等构造特征存在一定差异。

Based on many previous studies of the Buqin Mountain, A′nyêmaqên and Kuhai-Sêrtang ophiolitic mêlange zones in the junction between the two orogenic belts and through further survey and isotope chronological study, the authors find that the three ophiolitic mélange zones are not independent but form a typical triple junction with respect to the composition, textures and structures, geometry and isotope chronology, i.e. the Qinling-Kunlun triple junction.

本文在前人对发育于两造山带衔接区的布青山、阿尼玛卿以及苦海—赛什塘3条蛇绿构造混杂带大量研究的基础上,通过进一步的调查以及同位素年代学研究发现,这3条蛇绿构造混杂带并非相互独立存在,它们在物质组成、结构构造、几何形态、同位素年代学特征上构成较为典型的三向联结构造,即秦—昆三向联结构造。

Based on manifold materials of geophysical fetid, regional tectonics, surface activefaults, seismic activities and so on, we differentiated the seismotectonic belts in Chinamainland, and meanwhile, analyzed their active features and seismogenic tectonic conditions.

本文依据深部地球物理场、区域大地构造、地表活动断裂、地震活动等,划分了中国大陆的地震构造带,同时分析了地震构造带的活动特征和孕震构造条件。

The Namjagbarwa syntaxis consists of three tectonic units: the central Himalayan tectonic unit, and marginal Gangdise and Yarlung Zangbo tectonic units.

南迦巴瓦构造结由其核部的喜马拉雅构造单元和周边的冈底斯构造单元、雅鲁藏布构造单元组成。

The himalayan movement strengthened the south-directed thrusting and tectonic deformation intensity of Daba Mountain tectonic belt. In the process, Daba Mountain tectonic belt got the holding up by Michang Mountain and Huangling block ,then format the SW curvy extrusive structural features. Micang Mountain tectonic belt is a approximate autochthonous system that have small napping distance from north to south, suffered SN compression from Qinling leading to EW linear structure in himalayan.

喜马拉雅运动进一步加强了大巴山构造带向南的逆冲推覆和构造变形强度,在其推覆过程中受到米仓山近原地系统和黄陵地块的阻挡,形成如今向南西弧形突出的构造形迹;米仓山构造带是一近原地隆升系统,印支晚期以来的南北向挤压,形成东西向线性构造。

Applied the balanced cross-section technique to explain the characteristics of Kuqa rejuvenated foreland basin nappes and its structural shorten distance, and applied the structural triangle deposition bed discussed the time of structural deformation, that is structural deformation time in north older than in south area in Kuqa depression.

建立了库车再生前陆盆地6种局部构造变形的地质模型;利用平衡剖面技术解释了库车再生前陆冲断带,查明了构造变形特征和地层缩短量;研究了库车再生前陆盆地构造变形时间,探讨了前陆冲断带造山运动的特征和规律,指出库车前陆冲断带构造变形自北(25Ma)向南(2.5Ma)依次变新。

Determination of depth of granitic plutons was helpful for understanding of uplift of terranes and deep tectonism.

同时,构造地质学和大地构造学自身的研究也将不断拓宽研究领域①,如:1不断拓宽研究的时空尺度,深入了解地球早期构造作用和大陆地壳深部构造作用;2精确确定变形特征,特别是流变学特征,估算应变强度和流变学参数;3精细测定变形的时代,特别是早期变形的时间;4深入分析构造发生的动力源问题。

According to study the tectonic facies map of Balkhash- Junggar region, the article establishment geology conceptual model from two aspects which are tectonic setting and tectonic evolution. Based on the idea of information science, the article using Geodatabase data model and discussing feature class, attribute table and their mutual relations to construct tectonic facies spatial data model of Balkhash - Junggar region that based on the idea of information science.

闭于巴人喀什-准噶人地域大地构造相图入行剖析,自卑地构造空间序列和大地构造时光序列两个角度来树立地量概念模型,基于信做科教的念惟,当用Geodatabase数据模型,谈论大地构造相图的要荤类、属性外及其之间的互相闭解,构建基于信做科教念惟的巴人喀什-准噶人地域大地构造相图空间数据模型。

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客人们在卡罗利娜·埃凯家里,举止就文雅一些,因为卡罗利娜的母亲治家很严厉。

Designed by French fashion house Herm è s, this elegant uniform was manufactured in our home, Hong Kong, and was the first without a hat.

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