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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)
    The fluctuating on the isotherm plane is explained by surge, and the surge provided the academic foundation for the solidification control function.
    温度振荡现象的提出,解释了等温面上不同位置的波动现象,为结晶控制方程中的波动行为提供了理论依据。
    The second chapter's main contents include abstract the concept that is equal temperature area by according to character fuzzy zone ;
    第二章根据凝固前沿的物理特点,从稳态铸轧状态,抽象出铸轧区等温面概念;
    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。
    The extrapolation method of temperature and Heat flow Denisity atthe chamber surface has been estiblished on the basis of fundamental theo-ries of heat transfer. The temperature and heat flow Denisity on thechamber surface can be extrapolated from the measured temperature at theisothermic--Plane where the chamber surface is on a certain distance from.
    本文以热传导基本理论为基础,建立表面温度和表面热流密度的外推方法,可以根据离膛面某一距离等温面上的实测温度外推得到膛面温度和热流密度。
    Curie Point isother mal surface maps of Japan and of some regions in America and in China have been published. Some of the results are in agreement with regional variation in Pn velocity and some of them indicate a strong correlation between the spatial variation of the Curie isotherm level and the concentration of surface geothermal energy. They can also be used for the crust structure study.
    已发表了日本、美国及我国的部分地位的居里点等温面图,其結果某些与Pn波速的区域性变化相一致,某些指出居里等温面的空间变化与地热能面的集中密切相关,它们也可用于地壳结构的研究。
    On the basis of the above results,a preliminary analysis of the relations of isothermal surface of curie temperature and earthquake around the offshore Taiwan are presented.
    在此结果的基础上,对台湾周围海域的居里等温面及其与地震的关系作了初步探讨。
    Both analytical methods and numerical techniques showed thatthe instantaneous cooling rate causes the interface to become increasingly con-cave in Vertical Gradient Freeze Method. Dimensionless number D_e=R~2_ρc_pC. /〔k(T_h-T_o)〕is defined to express the extent that the interface becomesmore concave arised from instantaneous cooling rate.
    本文用解析和数值计算的方法,证明了静态温梯法晶体生长中,瞬时降温速率有使固液等温面下移且变得更凹的倾向,定义了降温显热数 De=R~2pc_pCo/k(T_h-T_c),用来表征瞬时降温速率使固液等温面变凹的程度。
 

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