Major Characteristics of the Lajishan Orogenic Belt of the South Qilian Mountains and Its Geotectonic Attribute

The Lajishan orogenic belt is one of the E-W-trending Caledonian erogenic belts within the Qinling-Qilian orogenic system. It was formed upon the Jiningian basement by intensive taphrogenesis. Its major characteristics comprise the prominent faulting along the north and south boundaries, the highly complicated petrological and petro-geochemical features of the volcanic rock series, and the development of a new type of ophiolite suite. In terms of tectonic analysis and the sequential analysis of tectonic settings of magmatic rocks, it is suggested that the Lajishan orogenic belt has undergone a complete "opening-closing" cycle, which can be further divided into 3 second-order "opening-closing" cycles. The composite characteristics of the "opening-closing" movement show that Laji Mountain is a typical fault orogenic belt. The fault orogenic belt is one of the most important types of intracontinental orogens. It is of critical theoretical and practical significance to summarize the characteristics and the     

略论重力在建立全球垂直基准中的作用

全球垂直基准与地球科学一全球变化的关系甚为密切,至于重力在其中的作用似乎应该到到进一步重视。为此,介绍了重力在确定高程,精化大地水准面中的作用和现状,研究和讨论了重力大地水准面的误差及可能达到的精度,阐明了精确确定Ｗ０,Ｕ０以及研究了重力场随时间变化在ＧＶＤ中的作用。     

APPLICATION OF THE HARTLEY TRANSFORM IN THE COMPUTATION OF THE GEOID IN CHINA

This paper presents a method for the computation of the Stokes for-mula using the Fast Hartley Transform（FHT）techniques.The algorithm is mostsuitable for the computation of real sequence transform,while the Fast FourierTransform（FFT）techniques are more suitable for the computaton of complex se-quence transform.A method of spherical coordinate transformation is presented inthis paper.By this method the errors,which are due to the approximate term inthe convolution of Stokes formula,can be effectively eliminated.Some numericaltests are given.By a comparison with both FFT techniques and numerical integra-tion method,the results show that the resulting values of geoidal undulations byFHT techniques are almost the same as by FFT techniques,and the computation-al speed of FHT techniques is about two times faster than that of FFT techniques.     

APPLICATION OF SEPARABILITY CRITERION IN DESIGN OF DEFORMATION MONITORING NETWORKS

A monitoring scheme must be so designed that several possible mod-els can be efficiently separated in the stage of analysis of deformation measure-ments.Based on the concept of separability developed by Chen and Chrzanowski,a methodology for the design of monitoring schemes has been developed by the au-thors.In the method a computer simulation technique is employed,into whichsome rules have been elaborated allowing minimal human intervention.In this pa-per the criterion is first presented and the design technique using the step one up-dating procedure is discussed.Finally,design of a simulated monitoring networkis made as a demonstrating example.     

A GEOMETRIC ALGORITHM FOR TILTED-CAMERA PERSPECTIVE PROJECTION AND THE COMPARISON WITH EXTERNAL PERSPECTIVE PROJECTION

A geometric algorithm for Tilted-Camera Perspective（TCP）projec-tion is proposed in this paper based on the principle of perspective projection.Ac-cording to that,the difference between TCP projection and External Perspective（EXP）projection is analyzed.It is put forward prerequisites making these twoprojections were compatible,and some examples are given.     

云南元江地区中元古代昆阳群下亚群的沉积地质及控矿作用

滇中地区昆阳群下亚群的沉积层序和沉积构型对原生铜矿形成、富集和就位均有重要的控制作用．从时间上讲,昆阳群下亚群分为４个层序．第一层序海侵体系域的因民组中上部火山岩和深水沉积及下伏大红山群为原生铜矿的生矿层,第一层序高水位体系域的落雪组及其上下过渡段为原生铜矿的储矿层,第二层序海侵体系域鹅头厂组的泥质沉积为铜矿的盖层．在空间上,滇中地区中元古代裂谷盆地的结构和沉积构型对铜矿的空间分布也具明显的控制作用．铜矿的就位场所主要位于断隆－断陷区之间的同沉积断裂附近,尤其是靠近断隆区边缘落雪组的高水位体系域进积序列及其相变带．元江地区中元古代的铜矿找矿方向应着重考虑同沉积断裂带与落雪组及上下过渡段相变的复合部位．     

隐伏地质异常地表间接显示模拟的遥感地质统计分析

根据隐伏地质异常表面产是接显示模拟实验的结果,经遥感地质定量分析表明,隐伏地质异常在地表的间接显示信息是以线性体复杂模式在被动遥感图像上得以显示的。     

Geodynamic Technique Applied to the Volcanic Activity Forecast of Lanzarote Island in Spain

In accordance with the Agreement of Sino-Spain Science and Technology Cooperation,the Institute of Seismology,SSB of China and the Institute of Astronomy and Geodesy of Spain have together performed research at the Geodynamics Laboratory of Lanzarote(Canary Islands)with geodynamic instrumentation.Researchers conducted observation and then analyzed the data compiled.Researchers using the advanced geodynamic instruments could monitor the volcanic activity and seismicity in order to forecast the volcanic eruption and earthquakes.The results of this paper are obtained from this scientific and technological cooperation of the two institutes between China and Spain.     

我国花岗斑岩中的铅猛钛铁矿

铅锰钛铁矿呈不规则粒状、片状产于内蒙古的花岗斑岩中。本文对该矿物作了电子探针分析,计算出其化学式并简化为(Pb,Na,K)(Ti,Fe,Zn,Mn)_(21)O_(38)。单晶X射线衍射结果表明它是三方晶系,空间群R3,晶胞参数a=10.378(13)A,c=20.809(15)A,Z=3。