中国地震报告数据处理系统

地震观测报告是一份具有广泛使用价值的地震基础资料。中国地震报告数据处理系统是提高中国地震报告质量的关键一环。其主要水平反映在:数据采集和处理自动化;采用最先进的数值计算方法;采用最先进的激光照排技术;用磁介质进行数据传递。     

STUDY OF NONLINEAR ROSSBY WAVES IN THE ATMOSPHERE UNDER SEMI-GEOSTROPHIC APPROXIMATION

Under semi-geostrophic approximation the nonlinear ordinary differential equations are obtained for the motion inthe barotropic and baroclinic atmospheres with the effects of zonal shear basic flow and topographic forcing included.Two constraints are acquired of finite-amplitude periodic and solitary waves in the original model with the aid of thephase-plane geometric qualitative theory of a dynamic system defined by the differential equation.The explicit solutionof the nonlinear waves is found by means of the approximation method and some significant results are achieved.     

单机地震数据采集系统NCDAS——华北地区遥测地震台网联网论文续一

设计了一套单机地震数据采集软件系统NCDAS.文中描述了该软件的总体结构、各任务块的功能、事件检测算法以及硬件环境.     

水震波异常与中期强震危险性关系初探

近年来在我国井网中发现某些强震之前井水位记震特性的异常现象。本文根据理论分析、试验研究与井网中统计结果提出水震波异常与区域应力状态的变化之间可能存在着一定关系,然后广泛收集了华北地区15口井水位1985—1991年间的水震波资料并系统分析了1989年10月19日大同—阳高M_s6.1地震前后井水位记震特性的变化,确认强震前存在着水震波异常。     

用于地球静止卫星云图象素定位的非线性插值法

根据对ＧＭＳ－４地球静止卫星所发定位网格数据的分析，发现同一纬线上两定位格点间象素分辨率的变化率基本保持不变。可以利用等比级数的原理计算象素分辨率，从而确定象素的地理位置。据此设计的非线性插值方法明显优于线性插值法。     

大气环流异常分析中使用合成方法的一个问题

通过一个实例的研究，指出，如果仅根据差值的绝对值大小来挑选关键区，其结果可能不可靠。它可能导致虚假的关键区或遗漏掉重要的关键区（在低纬度）。提出了解决问题的方法。     

松林冠层大气湍流结构观测研究

为了更好地了解大气与物质和能量交换，用二层三维超声风速温度仪测量了重庆市郊松林风速和温度脉动值。采样速率为每秒１次和１１次，数字量记录。计算了湍流动最通量和热通量的日变化，以及湍流风速的统计量和功率谱。结果表明，冠层上动量通量向下传输，而冠层内大多向上传输；冠层内湍流风速ｕ的三阶矩平均值大于零，ｗ的小于零；冠层上无因次湍流风速分量ｕ，ｗ标准差和无因次湍流动能耗散率与局地Ｍｏｎｉｎ－Ｏｂｕｋｈｏｖ长     

华北联网中心的短波天线：华北地区遥测地震台网联网论文续五

对华北联网中心北京中心短波天线的设计，功能，安装方案作了较为详细的介绍。     

The Sedimentary Sequence and Palaeogeographic Changes of the South Yellow Sea Since the Olduvai Subchron

According to the alternation of terrestrial beds and transgressive beds, the sedimentary sequence of the South Yellow Sea since the Olduvai subchron can be divided into 15 stratigraphical intervals. According to the facies analysis, there are 7 transgressive beds and one bed with transgression marks, and classical transgressive-regressive facies sequence also appears in the major transgressive beds.Palaeogeographic evolution in the shelf area involved 4 periods: (1) 1.70-0.5 Ma B. P. was the stage for the development of the Palaeo-Yangtze River alluvial plain and delta. Tide influenced -river channel sediments formed during the Olduvai have been found in borehole QC2. The river mouth was located near 124°E and during the transgressive stage from 0.97-0.73 Ma B.P. to the east of 122.2°E, a large-scale undersea delta was formed. In the regressive stage, the shelf area became an alluvial plain. (2) 0.50-0.75 Ma B.P. was a multi-transgressive fluctuation stage during which 3 transgressive beds (HVI, HV, H     

The PTst Evolution of Metamorphism and Development Mechanism of the Thermal-Structural-Gneiss Domes in the Chinese Altaides

A series of thermal-structural-gneiss domes (briefly TSG domes) are developed in the Chinese Altaides. Sericite-chlorite zone, biotite zone, garnet zone, staurolite zone, kyanite (andalusite)zone, sillimanite- cordierite (sillimanite-garnet)zone, migmatite zone and migmatic granite- gneiss field are developed from the low-grade metamorphic area to the centre of the TSG domes. The succession of the formation and evolution of the progressive metamorphic zone, migmatite zone and migmatic granite-gneiss corresponds to the spatial sequence from the outer part to the centre of the TSG domes. The peak temperature of the metamorphism and granitization increases progressively from 400℃ to 800℃ while the pressure decreases progressively from 1.05 GPa to 0.10 GPa from the biotite zone to the migmatic granite-gneiss field. The metamorphism of the erogenic belt may be described by the pressure-temperature-space-time model (PTst). In the main episode of orogeny, the deep heat flow and structural flow upsurged along