等温面

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。

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 .

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。

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 .

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。

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 .

塔里木盆地居里等温面特征及其地质意义

The characteristic and geological meaning of Curie isothermic surface under the Tarim basin

岩石圈居里等温面解释的若干问题

Some problems about interpretation of lithospheric Curie isothermal surface

京津唐地区居里等温面及其与地震的关系

Isothermal surface of Curie temperature around the Beijing area and its relation to earthquakes

台湾周围海域地区的居里等温面及其与地震关系的初步探讨

The preliminary analysis of isothermal surface of Curie temperature around the offshore Taiwan and its relations to earthquakes

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。

According to variable factors effecting temperature of lithologic Curie point , a method used to assent accuracy of Curie surface is given .

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。

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 .

应用三维磁性层反演理论和方法，对延庆、怀来地区航磁资料进行了数据处理，反演计算了该区磁性基底埋深、居里等温面埋深和视磁化强度分布。

Using 3-D magnetosphere inverse theory and method , we process the aeromagnetic data : of Yanqing and Huailai areas , and obtain the buried depth map of Curie isothermal surface and the distribution map of apparent specific magnetizing moment of these areas .

使用3次自然样条函数，将格点资料插值到每米的深度上，求出各格点28℃海温的深度，得出各月28℃等温包络面。

Interpolating sea temperature value at every meter by a spline function method , the depth with sea temperature of 28 ℃ and the envelope surface depth with constant temperature of 28 ℃ were obtained .

结果表明：4～11月份28℃等温包络面呈现大小不等和深浅不同的盆状，其各月的变化形象化地表示了暖水的演变过程。

It was found that from April to November , the 28 ℃ constant temperature envelope surfaces appeared like a pot pattern , with different size and depth , expressing the evolution processes of warm waters .

在等温热校形过程中，随着校正温度的提高，叶片校正效果越来越明显，当校正温度提高到900℃时，等温校正型面透光度最小；

In the isothermal adjustment , the improvement of blade profile become more and more obvious as the adjustment temperature increasing , mininum the transmissivity of blade profiles is reached when the adjustment temperature up to 900 ℃ .