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等温面     
相关语句
  isothermal surface
     SOME PROBLEMS ABOUT INTERPRETATION OF LITHOSPHERIC CURIE ISOTHERMAL SURFACE
     岩石圈居里等温面解释的若干问题
短句来源
     The authors of this paper discuss the deep structure characteristics of the Bohai Segruent of the TanLu fault in two aspects, e.g. the burried depth of the Curie isothermal surface and the crustal thickness.
     从居里等温面埋深和地壳厚度两方面论述郯庐断裂带渤海段的深部构造特征。
短句来源
     3. It will be seen on the section of the crust that the belt between the bottom of metamorphic rock of the Palaeozoic era and magnetic Curie isothermal surface is place of occurrence and brewing of earthquakes of the fracture belt.
     3.从地壳剖面上看,古生代变质岩系底板以下到磁性居里等温面之间的带状空间,是该断裂带的孕震和发震的层位。
短句来源
     Based on airborne magnetic data, the paper accounts Curie isothermal surface, and deals with the relationship of Curie isothermal surface and Moho surface, and its application on predicting the perspective of oil and gas.
     利用航磁资料计算了居里等温面,探讨了松辽盆地居里等温面与莫霍面的关系,以及在油气远景预测中的应用。
短句来源
     By using high precise aercamagnetic information and the method of frequency spectrum analysing, this papercalculated the Curie isothermal surface in the Hailar area which is between 12 to 28 km in depth,and then discussed the tensilegenesis mechanism and the interrelated character of rocks and its relation to tectonic movement.
     本文利用高精度航磁资料,应用谱分析方法,计算出海拉尔地区居里等温面深度介于2~18km之间,并据此探讨了海拉尔盆地的张性成因机制、岩相相关特征以及它与构造运动的关系。
短句来源
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  isothermic surface
     The characteristic and geological meaning of Curie isothermic surface under the Tarim basin
     塔里木盆地居里等温面特征及其地质意义
短句来源
     To produce the approximative mathematical model, at first,the structure of cabin according to isothermic surface is divided into many parts,and then considering every part as an isothermic body,its transmission function is deduced.
     建立近似数学模型的方法是,先把座舱结构按照等温面划分为许多部分,然后把每一部分看作一个等温体导出它的传递函数。
短句来源
     The depth of Curie isothermic surface (underneath depth of magnetic body) under the Tarim basin is obtained by taking the result of moment spectrum method as a restrictive model of Parker-Oldenburg method.
     利用矩谱法的计算结果作为Parker-Oldenburg方法的约束模型,计算了塔里木盆地居里等温面(磁性下界面)深度。
短句来源
  “等温面”译为未确定词的双语例句
     The deep structure of this earthquake has been discussed by analysis of seismic activity and macroscopic characteristics, combining with crustal thickness, the undulation of Curie's isotherm surface, the electrical structure of upper mantal of the crust and rock experiment material.
     本文从地震活动性、宏观特征分析开始,结合地壳厚度、居里等温面起伏以及地壳上地幔的电性结构和岩石实验材料,对这次地震的深部构造做了论述.
短句来源
     a high conductive asthenosphere with resistivity of one to several Ωm lays at a depth from 50 to 80 km beneath the plain and at a depth of more t han 100 km in the surrounding mountain regions, and it corresponds to the low velocity layer in the upper mantle determined by seismic methods.
     平原内上地幔高导层埋深50—80公里,山区大于100公里,与地震方法确定的上地幔低速层基本一致,同时与大地热流测量、居里等温面计算和对新生代玄武岩地球化学研究结果基本吻合。
短句来源
     According to variable factors effecting temperature of lithologic Curie point, a method used to assent accuracy of Curie surface is given.
     根据影响岩石居里点温度的各种因素,提出评估居里等温面计算精度的方法。
短句来源
     SOTHERMAL SURFACE OF CURIE TEMPERATURE IN FUJIAN AND ITS RELATION TO EARTHQUAKE
     福建地区的居里等温面及其与地震的关系
短句来源
     A CRUSTAL MAGNETIZATION MODEL AND CURIE ISOTHEM
     地壳磁化强度模型和居里等温面
短句来源
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  isothermal surface
The flow past a circular cylinder with an isothermal surface at Mach numbers M∞=2 and 5 and Reynolds numbers ranging from 104 to 108 is investigated on the basis of the Reynolds equations using a differential two-equation turbulence model.
      
Supersonic Flow Past a Circular Cylinder with an Isothermal Surface
      
Supersonic perfect-gas flow past a circular cylinder with an isothermal surface is investigated at the Mach number 5 and Reynolds numbers ranging from 30 to 500,000.
      
Results are given of numerical simulation of hydrodynamics and heat transfer under conditions of transverse flow past a two-dimensional "trench" (a groove whose cross section has the form of a segment of circle) located on a plane isothermal surface.
      
Results are given of numerical simulation of hydrodynamics and heat transfer under conditions of transverse flow past a two-dimensional "trench" (a groove whose cross section has the form of a segment of circle) located on a plane isothermal surface.
      
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  其他


The paper studies the spatial variation of the Curie point isotherms in Beijing-Tianjin-Tanshan area with the help of aeromagnetic data. The depth of this isothermal surface in different regions changes from 16 km to 26 km below sea level. It is shallower than those in the tectonic regions in other parts of China. It was found that the stress due to the difference of the temperature between two adjacent regions is very important for earthquake occurrence.

本文给出了京津唐地区居里等温面的计算结果。本区居里面的深度约为16—26公里。然后讨论了居里等温面与地震的关系,得出各地区之间地壳温度场的差异产生的应力可能是地震发生的一个重要原因。

The Beijing-Tianjin-Tangshan region and adjacent area are one of strong earthquake region in China and technically have undergone intense disturbance resulting in uprise of surrounding mountain regions and intensive fracture and subsidence of the plain since Cenozoic age. MT measurements at 30 sites have been carried out since 1976. Data of MT were processed by the tensor impedance method and the apparent resistivity curves of E polarization were fitted to 1-D models for obtainning the electrical structure of...

The Beijing-Tianjin-Tangshan region and adjacent area are one of strong earthquake region in China and technically have undergone intense disturbance resulting in uprise of surrounding mountain regions and intensive fracture and subsidence of the plain since Cenozoic age. MT measurements at 30 sites have been carried out since 1976. Data of MT were processed by the tensor impedance method and the apparent resistivity curves of E polarization were fitted to 1-D models for obtainning the electrical structure of the crust and upper mantle. The results of interpretation indicate that within the intermediate crust, there widely exists a high conductive layer with thickness of several km and resistivity from several to more than ten Ωm, and it corresponds to the low velocity layer in the crust determined by DSS; a high conductive asthenosphere with resistivity of one to several Ωm lays at a depth from 50 to 80 km beneath the plain and at a depth of more t han 100 km in the surrounding mountain regions, and it corresponds to the low velocity layer in the upper mantle determined by seismic methods. The variable tendency of the depth of high conductive asthenosphere receives a strong support from the heat flow measurements, Curie isothermic surface calculations and geochemical studies of the Cenozoic basalts. The strong shocks occurred there mainly along the margins of the uplift of the high conductive asthenosphere and the foci were located generally over the high conductive layer in the intermediate crust.

京津唐渤及其周围地区是我国的强烈地震活动区之一。自1976年以来,我们在该区开展大地电磁测深工作,完成了近30个测点。所得结果表明,本区壳内存在高导层,与地震方法确定的壳内低速层一致。平原内上地幔高导层埋深50—80公里,山区大于100公里,与地震方法确定的上地幔低速层基本一致,同时与大地热流测量、居里等温面计算和对新生代玄武岩地球化学研究结果基本吻合。本区绝大多数地震位于壳内高导层之上,强烈地震主要发生在上地幔高导层隆起的边缘。最后讨论了本区强震活动与壳内和上地幔高导层的关系。

On the basis of data on the gravity, the aeromagnetic survey, the apparent crustal thickness, the seismicity and the depth of focus, the author preliminarily studied and discussed the condition of fomation of the Xianshuihe frcture and relationship between it and occurrence of darthquakes. Results were showed as follows;1. As there was no clear and direct reflection of the Xianshuihe fracture on boundary surface between the crust and the mantle at the top of the mantle, this fracture may not pass through the...

On the basis of data on the gravity, the aeromagnetic survey, the apparent crustal thickness, the seismicity and the depth of focus, the author preliminarily studied and discussed the condition of fomation of the Xianshuihe frcture and relationship between it and occurrence of darthquakes. Results were showed as follows;1. As there was no clear and direct reflection of the Xianshuihe fracture on boundary surface between the crust and the mantle at the top of the mantle, this fracture may not pass through the lithosphere and was a strong regionnal fracture inside the crust.2. This fracture had devoloped on the tectonic background of upheaval of the crust before the Variscian period.3. It will be seen on the section of the crust that the belt between the bottom of metamorphic rock of the Palaeozoic era and magnetic Curie isothermal surface is place of occurrence and brewing of earthquakes of the fracture belt.4. Because of irruption of magmas or fluids with high temperature, upheaval and higher temperature sites on magnetic Curie isothermal surface usually are the bottom of fractures brewing earthquake. Because temperature of the bottom is raised and the upside is caught here, the stress is concentrated easily and movement of the fracture easily is caused, therefore it is principal place where strong earthquakes brew and occur.

本文根据重力、航磁、地壳视厚度、地震活动性及震源深度等资料,对鲜水河断裂带形成的深部状况及其与地震发生的关系进行了初步分析和讨论。结果表明: 1.该断裂带在上地幔顶部的壳幔界面上並未得到清晰和直观的反映,因此推测它可能未切穿岩石圈,而属一条壳内区域大断裂。2.该断裂是在前海西期构造隆起背景上发育起来的。3.从地壳剖面上看,古生代变质岩系底板以下到磁性居里等温面之间的带状空间,是该断裂带的孕震和发震的层位。4.磁性居里等温面的隆起或高点部位,因岩浆或高温流体的侵入,往往是孕震断层的根部,根部增温,上部锁住,故有利于应力的集中,最易产生错动,而成为强震孕育、发生的重要场所。

 
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