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tectonic style
相关语句
  构造样式
    FAULT SYSTEM AND TECTONIC STYLE OF THE YITONG GRABEN
    伊通地堑断层系统与构造样式
短句来源
    On the background of the mineral deposit geology and geochemistry,the tectonic style and the tectonic stress field during the gold mineralization are studied,and based on the Acoustic Emission stress measurements,the tectono physical model is set up.
    在矿床地质和地球化学背景上,对成矿过程中的构造样式及构造应力场进行研究,采用声发射地应力等方法建立了矿田的构造物理模型。
短句来源
    Strike-slip basins are commonly complex, mainly because of its complicated fault system and tectonic style.
    与走滑相关的盆地构造一般比较复杂,主要表现为断层系统较复杂和构造样式类型丰富。
短句来源
    Guided by the theory of fault-related fold,tectonic geometry along with tectonic kinematics,the tectonic models are established from surface and drilling data,the fine tectonic interpretation is implemented and the tectonic 3D distribution is analyzed based on the analysis of tectonic style and decollement layers.
    以断层相关褶皱理论、构造几何学、构造运动学为指导,在分析构造样式、滑脱层系的基础上,结合地表、钻井资料建立了构造模型,进行构造精细解释,分析了构造的三维展布特征。
短句来源
  构造样式
    FAULT SYSTEM AND TECTONIC STYLE OF THE YITONG GRABEN
    伊通地堑断层系统与构造样式
短句来源
    On the background of the mineral deposit geology and geochemistry,the tectonic style and the tectonic stress field during the gold mineralization are studied,and based on the Acoustic Emission stress measurements,the tectono physical model is set up.
    在矿床地质和地球化学背景上,对成矿过程中的构造样式及构造应力场进行研究,采用声发射地应力等方法建立了矿田的构造物理模型。
短句来源
    Strike-slip basins are commonly complex, mainly because of its complicated fault system and tectonic style.
    与走滑相关的盆地构造一般比较复杂,主要表现为断层系统较复杂和构造样式类型丰富。
短句来源
    Guided by the theory of fault-related fold,tectonic geometry along with tectonic kinematics,the tectonic models are established from surface and drilling data,the fine tectonic interpretation is implemented and the tectonic 3D distribution is analyzed based on the analysis of tectonic style and decollement layers.
    以断层相关褶皱理论、构造几何学、构造运动学为指导,在分析构造样式、滑脱层系的基础上,结合地表、钻井资料建立了构造模型,进行构造精细解释,分析了构造的三维展布特征。
短句来源
  “tectonic style”译为未确定词的双语例句
    Based on their size,total displacement and tectonic style,basins of the Fenwei graben system(northeast of China)can be divided into four types,the infant(or initial),the young(or growing),the mature and the joining ones,each succeeding stage being developed from the preceding one.
    基于盆地断陷规模、断陷幅度、构造样式的差异 ,将汾渭地堑系诸盆地划分为初始型、成长型、成熟型及连接型四类 ;
短句来源
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  tectonic style
Similarly, the details of plate tectonic modalities (plate size, plate motion rate, plate thickness, tectonic style, irregular crustal growth, etc...) were different of modern plate tectonics.
      
The tectonic style of a terrestrial planet depends strongly on the mechanisms of heat release from the mantle through the lithosphere to the surface.
      
Today one of the main questions standing before geology of Venus is comprehension of tectonic style on surface of this planet.
      
These factorsinfluence the mechanical properties of the lithosphere across thediscontinuity, and ultimately the tectonic style of the NTD that can besupported.
      
Swath bathymetry and sidescan data, together with seismic reflection and geopotential data obtained during the GEODYNZ-SUD cruise, showed major changes in tectonic style along the margin.
      
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The Jinchanggouliang gold deposit located in the northern margin of the North China Block occurs where the Late Archean gneiss was invaded by the hypabyssal subhypabyssal porphyritic granite stock during 126.3-121.5Ma.Vein golds were formed when magmatic hydrothermal liquids injected into the radial and conjugate fractures around the stock during 121.7-100.02Ma.On the background of the mineral deposit geology and geochemistry,the tectonic style and the tectonic stress field during the gold mineralization...

The Jinchanggouliang gold deposit located in the northern margin of the North China Block occurs where the Late Archean gneiss was invaded by the hypabyssal subhypabyssal porphyritic granite stock during 126.3-121.5Ma.Vein golds were formed when magmatic hydrothermal liquids injected into the radial and conjugate fractures around the stock during 121.7-100.02Ma.On the background of the mineral deposit geology and geochemistry,the tectonic style and the tectonic stress field during the gold mineralization are studied,and based on the Acoustic Emission stress measurements,the tectono physical model is set up.It is suggested that the uplift denudation process of the basement rock of the ore deposit from the depth of 9.1km to the surface and the emplacement of the small stocks at the depth of 3.4km are closely related with the Meso Cenozoic tectonic movement of the East Asia Peri Pacific tectonic mineralization domain.

华北克拉通北缘的金厂沟梁金矿产于晚太古宙片麻岩系中,126.3—121.5Ma的浅成相斑状花岗岩岩株侵位,121.71—100.02Ma在岩株周边的放射状—共轭断裂中,岩浆热液注入形成脉状金矿。在矿床地质和地球化学背景上,对成矿过程中的构造样式及构造应力场进行研究,采用声发射地应力等方法建立了矿田的构造物理模型。6期构造应力场表明矿床所在基底岩块自9.1km深处抬升,在3.4km处小岩株侵位直到剥蚀浮升到地表的过程是与东亚滨太平洋构造成矿域中、新生代活动密切联系的。

Based on their size,total displacement and tectonic style,basins of the Fenwei graben system(northeast of China)can be divided into four types,the infant(or initial),the young(or growing),the mature and the joining ones,each succeeding stage being developed from the preceding one. From the infant basin through the young or the mature,there was a decline in the structure barrier(or the resistance of the basin to further depression or expansion)resulting in a decrease of the upper limit of earthquake magnitude....

Based on their size,total displacement and tectonic style,basins of the Fenwei graben system(northeast of China)can be divided into four types,the infant(or initial),the young(or growing),the mature and the joining ones,each succeeding stage being developed from the preceding one. From the infant basin through the young or the mature,there was a decline in the structure barrier(or the resistance of the basin to further depression or expansion)resulting in a decrease of the upper limit of earthquake magnitude.

基于盆地断陷规模、断陷幅度、构造样式的差异 ,将汾渭地堑系诸盆地划分为初始型、成长型、成熟型及连接型四类 ;认为盆地从初始型、成长型至成熟型 ,其构造闭琐度有减弱的趋势 ;剖析了各级强震震源区的构造特征 ,依据震源体理论 ,认为盆地类型与震级上限有对应关系。

Based on the thinking of layered blocked structure of the Earth, a structural analysis has been made for the tomography of the natural seismic surface wave in South China region, and high speed blocks varying in shape and differing in size have been discovered in the lower lithosphere, which are termed mantle blocks, on the basis of the studies of the geological, geochemical and geophysical signs. It is showed that the tectonic pattern of the South China lithosphere and the superficial deformation...

Based on the thinking of layered blocked structure of the Earth, a structural analysis has been made for the tomography of the natural seismic surface wave in South China region, and high speed blocks varying in shape and differing in size have been discovered in the lower lithosphere, which are termed mantle blocks, on the basis of the studies of the geological, geochemical and geophysical signs. It is showed that the tectonic pattern of the South China lithosphere and the superficial deformation are basically controlled by the high speed blocks or the mantle blocks. Based on the systematic 3D studies of the high speed blocks in the lithosphere, three 3D geometric tectonic styles (craton root shaped, orogen wedge shaped, and clastic massive) are formulated for the first time, and three tectonic evolution types of the lithospheres (cratonic, thickening and thinning) are divided. From the 3D geometric models of the lithosphere and asthenosphere in the south China region, the evolution pattern of the lithosphere is deduced.

从地球层块结构研究思路出发,对华南及邻区天然地震面波层析成像进行系统地构造解析,发现岩石圈中下部存在形态各异,大小不等的高速块体,结合地质学、地球化学、其它地球物理学标志等多学科综合研究,将其称为幔块构造。研究显示高速块体或幔块构造是华南地区岩石圈构造格局和岩石圈表层构造变形最基本条件之一。首次建立起华南地区岩石圈三种三维几何结构样式:克拉通陆根状结构、造山带楔状结构和碎块状结构,以及岩石圈三类构造演化类型:克拉通型岩石圈、增厚型岩石圈和减薄型岩石圈(弱减薄型岩石圈及强减薄型岩石圈)。本文在论述华南岩石圈三维结构构造类型基本特征基础上,首次探讨了华南地区软流圈三维结构以及该区岩石圈演化动力学特征。

 
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