深部构造表现为断裂构造和特有的地壳结构。
The deep structure displays the fault structure and the characteristic crustal architecture.
结果显示上部地壳结构总体上横向比较均匀，纵向分层明显。
The results show that the upper crustal structure is relatively well-distributed laterally and obviously by layers vertically.
极移是以可预见的方式行进着，现有的地壳结构创作了这场戏剧。
The pole shift proceeds in a predictable fashion, the existing structure of the crust scripting this drama.
中国大陆边缘和西太平洋洋壳之间的黄海海域，属于过渡型地壳结构。
Yellow Sea area, located between the margin of China's mainland and the oceanic crust of the Western Pacific ocean, has transitional crustal structure.
中国大陆边缘和西太平洋洋壳之间的黄海海域，属于过渡型地壳结构。
Yellow Sea area, located between the margin of China's mainland and the oceanic crust of...
文章利用天然地震的PS转换波研究了北部湾陆缘地区的地壳结构特征。
By the data of PS-waves of the earthquakes, the crustal structure of the margin of the Beibu Gulf is studied in this paper.
总体北倾的莫霍面和同样北倾的下地壳结构记录了中生代扬子陆块的向北俯冲。
The North-dipping structure recorded northward subduction of the Yangtze block happened in Mesozoic.
同类盆地的油气丰度有巨大差异的主要原因可能与地壳结构特征的差别有密切关系。
The differences of similar basins in oil-potential and gas-potentials are mainly caused by the differences in the crustal structures.
由于碰撞造山带具有的地壳结构的复杂性，必须采用新的研究方法来分析其热结构。
Because a collision orogenic belt has a complicated crustal structure, new methods have to be adopted for thermal state analysis.
上述三种类型地壳结构的差异，主要是由上地幔物质向地壳的垂直迁移程度不同造成的。
The difference between different crustal structures may be largely due to the difference in degree of vertical migration of-materials from the uppermost mantle into the crust.
它们不仅在地表形成了三山两盆的盆山结构面貌，而且在深部的地壳结构上也有明显的不同。
The transect not only displays the style of basin-mountain tectonics, with three mountain ranges and two basins on the surface, but also reveals different crustal structures in different parts.
过去的月震研究最主要的限制就是去除噪声，这些噪声由迭加信号在月球的分馏地壳结构中反复反射引起。
A primary limitation to past lunar seismic studies was the wash of'noise' caused by overlapping signals bouncing repeatedly offstructures in the Moon’s fractionated crust.
近十年来，深地震反射波勘探在海洋岩石圈的形成与演化、地壳结构研究中的应用越来越广泛。
In the recent decade, the deep seismic reflection profiling has been applied widely to studies on formation and evolution of oceanic lithosphere, crust structures and so on.
结果表明两大构造单元基底的岩石波速差异较大，从而认为两者物质组成迥异，地壳结构完全不同。
As a result, the wave velocity of the two structural units are different obviously, so we think there is great difference in the constituted materials, and the crust structures are entirely different.
本文利用重力资料计算了华北地区康氏面和莫氏面的深度，从而得出了这一地区地壳结构的基本形态。
Using gravity data the depths of Moho and Conrad discontinuities in North China region are calculated and thus the basic configuration of crustal structure in this region can be determined.
并从重力场反映的地壳结构、地壳形变、地壳应力状态、地壳活动性诸方面，论述了各构造区的特征。
He describes features of tectonic regions, including crustal structure, crustal deformation, stress field and crustal activity.
概述了近年来用近垂直反射地震方法研究不同大地构造单元的地壳结构和深部构造问题所取得的基本成果。
The paper summarizes the basic achievement in studying the crustal structure and deep tectonics of different geotectonic unit by near normal seismic reflection in recent years.
在研究地壳结构的人工源宽角反射地震资料解释中，常规宽角反射波走时和射线路径计算大都假定地壳模型为层状块状均匀介质。
Layered and blocked homogeneous models are usually used to calculated travel times and ray paths of wide-angle reflection waves in interpreting wide-angle reflection data of deep seismic sounding.
但它们形成的时代不同，沂沭裂谷已经消亡，里奥格兰德裂谷是现代裂谷，因此它们在现代构造、地壳结构、地震活动等方面不同。
The Yishu rift-valley has been died out and the Rio Grande rift-valley is a modern rift-valley. Thercfore they are different in modern tectonics, crustal structure and seismic activity.
已有资料表明，在中国西北盆山地区，山脉和盆地具有明显不同的地壳结构，它们的地壳厚度不同，表现为山区地壳厚，具有明显的山根；盆地区地壳厚度小。
Based on the data of the Xinjiang Geotransect and other related geotransects, the crustal tectonics of the basin-mountains area in northwestern China are discussed in this paper.
本文讨论了金属矿产资源与地壳、地幔结构及深部物质运移的动力学响应。
Dynamic response of metallic mineral resources and crust, mantle structure and deep substance migration is discussed in this paper.
研究结果表明，地壳深部结构与地震活动存在着一定的联系。
The results suggest that there exist a certain relation between deep crustal structure and seismic activity.
本文是研究利用天然地震PS转换波及PPP等二次波到时资料反演地壳上地幔速度结构的尝试。
An inversion of velocity structure of crust and upper mantle by using converted PS wave and multiwave PPP etc, is reported in this paper.
结合区域岩石圈结构，上述特征表明花岗岩源岩应为中地壳结晶片岩、片麻岩。
According to all above characteristics and regional lithospheric structure, the granites should come from schist and gneiss of middle crust.
结果表明，既使在较稳定的地台区，地壳内部的结构也可能是相当复杂的。
The results also indicate that even in a more stable platform area, the structure of the crust interior can also be quite complicated.
区域地震波携带着大量的信息，可以很好地反映地壳和上地幔结构的变化。
Regional seismic wave carries lots of information about structural variations in the crust and the upper mantle.
用近震资料能得到在水平向和垂直向分辨率较高的地壳速度结构。
The better resolution in horizontal and vertical compenents for the crustal velocity structure can be obtained by using local earthquake data.
用近震资料能得到在水平向和垂直向分辨率较高的地壳速度结构。
The better resolution in horizontal and vertical compenents for the crustal velocity structure can be obtained by using local earthquake data.
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