tectonic stress信息详情
[地物][力]构造应力
stress───n.压力;强调;紧张;重要性;重读;vt.强调;使紧张;加压力于;用重音读;n.(Stress)人名;(意)斯特雷斯
plate tectonic───板块构造
alternating stress mean stress───交变应力平均应力
shear stress───[力]剪应力;[力]剪切应力;剪应力; 切变应力; 切应力; 粘性摩擦应力
tectonic plate───地壳构造板块;[物][构造]板块
tectonic plates───(地球表面的)构造板块
financial stress───资金紧张;财务压力
residual stress───[力]剩余应力;残余应力
M stress───M应力
The primary analysis considered the effect could be relative to tectonic stress field.───初步分析认为,这种现象可能与现代构造应力场有关。
The tectonic stress the Earth are mainly on the upper lithosphere.───地球内部构造应力主要集中于岩石圈上层。
The contemporary tectonic stress field inherites the one in Late Pleistocene.───现今构造应力场继承了更新世以来的构造应力场;
The stress's size distribution is controlled by fault distribution, burial depth and the size and direction of the tectonic stress.───地应力大小分布主要受控于断层展布、地层埋深及构造应力大小和作用方位。
During the rise of plateau, the tectonic stress on the marginal zone along the two sides accumulated in a long term.───在青藏高原隆升的过程中,两侧边缘带构造应力长期积累。
There exist a complex brittle fracture system and a tectonic stress field within 2000 m of the main hole.───在主孔2000米之内,存在复杂的脆性破裂系统和构造应力场。
The structural pattern of block J is related to its tectonic background, basement topography and tectonic stress.───J区块这一构造特征与其所处的构造背景、基底形态和构造应力作用有关。
The change of the P wave velocity from upper crust to lower crust is consistent with the evolution history of the tectonic stress filed.───从上到下的速度等值线走向变化体现了该地区的构造应力场演化历史;
Deformation pattern of rocks in earth's crust is effected by tectonic stress, fluid pressure and gravity of the overlying strata.───地壳中岩石的变形模式受构造应力、流体压力和上覆岩层重力共同作用的影响。
Recent tectonic stress field is entirely dominated by the principal compressive stress with the components, whose orientation is in level, approximate level or sideling direction.
The Mesoproterozoic tectonic stress field could be simulated on the analysis of the distribution and mechanical origin of the Mesoproterozoic mafic dyke swarms in the central NCC.
During the rise of plateau, the tectonic stress on the marginal zone along the two sides accumulated in a long term.
And the character of faults is determined by the space state of tectonic stress fields.
Now, theprecise analytical of tectonic stress can't be given due to many fuzzy influent factors.
The later character should be attributed to the combined action of darn site's geomorphology and horizontal tectonic stress conditions, and is also influenced by the regional geostructural fractures.
The force source of current tectonic stress field comes mainly from the westward and northwestward horizontal extrusions from the Pacific and Philippine Plates respectively to the Eurasian Plate.
In extensional tectonic stress field, there are paralleling and ring - radiating fault block modes.
The tectonic stress the Earth are mainly on the upper lithosphere.
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