1) Curie surface
居里面
1.
Then we use field separation and Curie isothermic surface inversion in frequency domain to obtain the Curie surface map in depth.
本文对航磁数据进行延拓、方向导数和小波多尺度分解等各种处理,获得了该区的断裂体系分布,同时还提取了与居里面有关的区域场并反演了居里等温面,得出了该区居里面深度图。
2.
On the basis of qualitative analysis of the aeromagnetic anomaly and geologic structure features in Qinghai-Tibet plateau, the buried depth of Curie surface in the plateau is quantitatively computed by using 3-D magnetic layer inversion method in frequency domain.
在对青藏高原航磁异常及地质构造特征进行定性分析的基础上 ,利用频率域三维磁性层反演方法对青藏高原居里面埋深进行了定量计算。
3.
Some convertional methods were also applied to the study, which were reduction to the pole, upward continuation, vertical and horizontal derivatives, apparent magnetic susceptibility mapping and Curie surface and the depth-to-basement determination.
利用高精度航磁资料采用对应分析、图像处理、人机交互等新方法及各种常规处理手段，并结合地质和其它地球物理资料对研究区结晶基底的起伏状态、性质、居里面起伏变化特征以及深部断裂构造的展布格局等作了研究；计算了该条带域地壳磁层上、下界面深度；圈定了各类火成岩体的分布范围以及不同级次的断裂构造１１条；指明了基底岩相的分布特征；阐述了结晶基底以及居里面起伏变化特征，并对该条带域油气远景作出了评
2) Courier interface
居里界面
3) depth of Curie interface
居里面深度
4) Curie isothermal surface
居里等温面
1.
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。
2.
This paper introduces some methods which are applicated to calculate Curie isothermal surface by regional magnetic date.
介绍了利用区域磁测资料计算居里等温面的几种常用方法。
5) Curie isotherm
居里等温面
1.
Methods of mapping the depth to the Curie isotherm;
居里等温面深度的探测方法(英文)
补充资料：不看金面看佛面
1.同"不看僧面看佛面"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条