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    SOME PROBLEMS ABOUT INTERPRETATION OF LITHOSPHERIC CURIE ISOTHERMAL SURFACE
    岩石圈居里等温面解释的若干问题
    The results show that the depth of basement magnetic interface in Dongpu Depression is 12km deep, the lower Curie isotherm surface uplifts and the depression interior is filled by weak magnetic mass.
    结果显示东濮凹陷基底磁性界面深达12km,下部居里等温面上隆,凹陷内被弱磁性物质填充。
    ISOTHERMAL SURFACE OF CURIE TEMPERATURE AROUND THE BEIJING AREA AND ITS RELATION TO EARTHQUAKES
    京津唐地区居里等温面及其与地震的关系
    CURIE ISOTHERMAL SURFACE AND HEAT FLOW ANALYSIS OF THE ADJACENT REGION OF THE NIANQING TANGGULA PIEDMONT FAULTED ZONES
    念青唐古拉山前断裂系周围地区的居里等温面与热流分析
    THE PRELIMINARY ANALYSIS OF ISOTHERMAL SURFACE OF CURIE TEMPERATURE AROUND THE OFFSHORE TAIWAN AND ITS RELATIONS 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
    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
    CALCULAING CURIE ISOTHERMAL SURFACE IN THE HAILAR AREA BY AERO-MAGNETIC INFORMATION
    利用航磁资料计算海拉尔地区居里等温面
    A CRUSTAL MAGNETIZATION MODEL AND CURIE ISOTHEM
    地壳磁化强度模型和居里等温面
    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
    Methods of mapping the depth to the Curie isotherm
    居里等温面深度的探测方法(英文)
    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。
    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。
    The depth of the Curie isothemal surface of this area has been calculated from the aeromagnetic anomalies.
    该区的居里等温面深度约16公里,地温梯度达40℃/公里以上,热流值达2.5HFU以上。 可以认为,这是羊八井地区热田的深部热源。
 

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